REG - Castillo Copper Ltd - Encouraging REE metallurgy test-work from BHA
28/02/2023 07:00
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RNS Number : 2178R Castillo Copper Limited 28 February 2023
28 February 2023
CASTILLO COPPER LIMITED
("Castillo", or the "Company")
Encouraging REE metallurgy test-work from Broken Hill
Castillo Copper Limited (LSE and ASX: CCZ), a base metal explorer primarily
focused on copper across Australia and Zambia, is pleased to announce
encouraging results from initial Rare Earth Element ("REE") metallurgical
test-work at the Fence Gossan Prospect (Appendix A) within the BHA Project's
East Zone.
HIGHLIGHTS:
· Preliminary metallurgical test-work on a 20m composite sample from
the Fence Gossan Prospect (FG_003RC) delivered encouraging results, with clays
- subjected to froth flotation - obtaining up to 2-3 times REE enrichment from
the head grade at up to 70% recovery (refer Figure 1 and Appendix B for full
details):
o These findings confirm REEs can be readily separated from clay within the
East Zone discovery area and potentially beneficiated to a higher grade
concentrate
· To acquire a deeper understanding of the potential to extract
REE-mineralisation from clays in the East Zone discovery area, the Board has
approved appointing a specialist consultancy to conduct an in-depth metallurgy
test-work programme:
o Once completed and interpreted, the results from this programme will be
key to securing interest from potential off-take partners and providing a path
to market
· Further, 1m re-assays for Reefs Tank were received for all four
drill-holes (RT_001-4RC), which further verified there is an extensive,
shallow REE system apparent across the central part of the East Zone - the
best intercept comprised:
o 3m @ 2,587ppm TREO from 14m (RT_001RC)
· Reconciling all assays from the recent drilling and auger campaigns
across the Fence Gossan, Tors and Reefs Tanks Prospects, the geology team has
created heat maps which identify zones of high Total and Magnetic Rare Earth
Oxides ("TREO"/"MREO"):
o These areas will be subject to further surface sampling and geophysical
surveys then potentially drill-testing to extend known mineralisation
Ged Hall, Chairman of Castillo Copper, said: "On a holistic basis, the Board
is delighted with results from the drilling, surface sampling and
metallurgical test-work at Broken Hill as they collectively demonstrate the
forward value creating potential of the BHA Project's East Zone. In short, the
underlying REE system is shallow, extends over at least 4.5km(2), delivered
results up to 3,491ppm TREO and produced up to 38.9% MREO in diamond core(1).
Moreover, the metallurgy test-work proves REE mineralisation readily separates
from clay and can potentially be beneficiated to a higher-grade concentrate.
By all accounts, this is an excellent report card ahead of exploratory work
ramping up."
ENCOURAGING METALLURGICAL TEST-WORK RESULTS
FIGURE A1: HEAD ASSAY / IMPROVEMENT
ANALYTE ALS Adelaide ALS Perth Times Improvement
REE ME-MS81 HEAD GRADE REE COMP %
%
Ce (%) 0.045 0.05 1.6
La (%) 0.038 0.03 2.3
Nd (%) 0.021 0.02 2.0
Pr (%) 0.006 0.01 1.3
Y (%) 0.009 0.01 1.1
Source: ALS
To follow up on these excellent results, the Board has now approved the
appointment of a specialist metallurgy consultancy with extensive experience
in how REE mineralisation liberates from various host rocks (including clays).
The Board wants a deeper understanding of the potential to extract REE
mineralisation from the East Zone discovery area, as this information will be
key to securing interest from potential off-take partners that can provide a
clear path to market.
Reefs Tank Assays
All 1m re-assays for Reefs Tank were received for the four drill-holes
(RT_001-4RC), with up to 2,587ppm TREO recorded (Figure 1). On a holistic
basis, the Reefs Tank results provide incremental evidence there is an
extensive, shallow REE system apparent across the central part of the BHA
Project's East Zone (Appendix A).
FIGURE 1: REEFS TANK 1M ASSAYS
Hole From (m) To (m) Width (m) Ag Th (ppm) U (ppm) TREO (ppm) TREO-Ce (ppm) LREO (ppm) HREO (ppm) CREO MREO
(g/t) (%) (%)
RT_001RC 11 13 2 0.05 17.0 5.4 631 313.08 490.55 140.69 27.3% 20.6%
RT_001RC 14 17 3 0.96 29.9 9.4 2,587 2187.30 1105.24 1481.70 55.7% 24.7%
RT_001RC 54 55 1 0.15 70.2 9.2 796 429.43 746.15 49.34 20.8% 29.1%
RT_001RC 55 56 1 0.08 80.5 6.2 896 487.84 838.19 57.49 21.2% 29.9%
RT_001RC 64 65 1 0.12 121.0 9.0 1,236 658.75 1196.01 40.09 19.0% 29.3%
RT_002RC 0 1 1 0.06 19.8 2.5 367 241.55 272.76 94.70 34.1% 28.2%
RT_002RC 1 4 3 0.11 24.7 2.5 449 285.00 350.63 98.36 31.5% 27.6%
RT_002RC 28 32 4 0.12 54.6 3.5 601 343.27 541.76 59.48 24.1% 30.9%
RT_002RC 64 68 4 0.05 27.6 3.2 430 267.15 339.41 90.36 30.7% 27.5%
RT_003RC 0 4 4 nd 14.6 6.2 247 165.15 183.62 63.40 34.5% 29.8%
RT_003RC 8 16 8 nd 27.5 4.5 424 258.35 352.12 71.76 28.4% 28.5%
RT_003RC 56 64 8 nd 23.8 3.8 389 237.70 313.43 75.97 29.6% 27.6%
RT_003RC 72 76 4 nd 28.6 6.9 450 272.82 366.14 83.72 29.1% 27.3%
RT_004RC 52 56 4 0.25 44.4 4.1 567 344.40 465.92 101.13 29.1% 29.2%
RT_004RC 84 92 8 1.78 25.6 8.5 525 314.92 433.13 92.23 28.4% 27.7%
Source: CCZ geology team
TREO / MREO Contours
After reconciling all assays from the recent drilling and auger campaigns
across the Fence Gossan, Tors & Reefs Tanks Prospects (Appendix B), the
geology team has created heat maps which identify zones of high TREO and MREO
(Figure 2 & 3).
These areas will be subject to further surface sampling and geophysical
campaigns (including trial transects of ground radiometric and EM surveys)
then potentially drill-testing (red zones in Figure 2) to extend known
mineralisation.
Note, the TREO is the sum of REEs in ppm, calculated from ME-MS81 method,
converted to their stoichiometric equivalent i.e., Ce converted to CeO(2) and
so forth. The high-value Magnetic REO comprise Nd+Pr+Dy+Tb and generally
command premium pricing to other REEs as they are in strong demand. Refer to
Appendix C for a full explanation and TREO calculation.
FIGURE 2: FENCE GOSSAN AND SURROUNDS SURFACE SAMPLING - TREO IN PPM
Source: CCZ geology team
FIGURE 3: FENCE GOSSAN AND SURROUNDS SURFACE SAMPLING - MREO ppm
Notes: All coordinates in MGA94-Z54S Source: CCZ Geology team
For further information, please contact:
Castillo Copper Limited +61 8 6558 0886
Dr Dennis Jensen (Australia), Managing Director
Gerrard Hall (UK), Chairman
SI Capital Limited (Financial Adviser and Corporate Broker) +44 (0)1483 413500
Nick Emerson
Gracechurch Group (Financial PR) +44 (0)20 4582 3500
Harry Chathli, Alexis Gore, Henry Gamble
About Castillo Copper
Castillo Copper Limited is an Australian-based explorer primarily focused on
copper across Australia and Zambia. The group is embarking on a strategic
transformation to morph into a mid-tier copper group underpinned by its core
projects:
· A large footprint in the Mt Isa copper-belt district, north-west
Queensland, which delivers significant exploration upside through having
several high-grade targets and a sizeable untested anomaly within its
boundaries in a copper-rich region.
· Four high-quality prospective assets across Zambia's copper-belt
which is the second largest copper producer in Africa.
· A large tenure footprint proximal to Broken Hill's world-class
deposit that is prospective for zinc-silver-lead-copper-gold and platinoids.
· Cangai Copper Mine in northern New South Wales, which is one of
Australia's highest grading historic copper mines.
The group is listed on the LSE and ASX under the ticker "CCZ."
Competent Person's Statement
The information in this report that relates to Exploration Results and Mineral
Resource Estimates for "BHA Project, East Zone" is based on information
compiled or reviewed by Mr Mark Biggs. Mr Biggs is a director of ROM
Resources, a company which is a shareholder of Castillo Copper Limited. ROM
Resources provides ad hoc geological consultancy services to Castillo Copper
Limited. Mr Biggs is a member of the Australian Institute of Mining and
Metallurgy (member #107188) and has sufficient experience of relevance to the
styles of mineralisation and types of deposits under consideration, and to the
activities undertaken, to qualify as a Competent Person as defined in the 2012
Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for
Reporting of Exploration Results, and Mineral Resources. Mr Biggs holds an
AusIMM Online Course Certificate in 2012 JORC Code Reporting. Mr Biggs also
consents to the inclusion in this report of the matters based on information
in the form and context in which it appears.
References
1) CCZ ASX Release - 15 February 2023
APPENDIX A: BHA PROJECT'S EAST ZONE
FIGURE A1: BHA PROJECT's EAST ZONE - REE EXPLORATION FOOTPRINT
Source: CCZ geology team
FIGURE A2: BHA PROJECT
Source: CCZ geology team
APPENDIX B: PRELIMINARY METALLURGY TESTWORK
Background and Scope
A composite sample of RC chips from Fence Gossan drill-hole FG_003RC was
constructed over the interval from 0-20m. The material reported over that
interval had lithology logged as clay, haematite, goethite, and extremely
weathered pegmatite. The main rare-containing minerals are thought to be
monazite, allanite, xenotime, and possibly baryte or celsian (to account for
the high barium contents of some samples). Note, these assumptions need to be
tested by XRD and/or QEM-SEM testing.
The composite was made up of 1m samples tested using ME-MS81 analysis method
(the results for which are provided in Figure A1).
The process methodology followed by ALS Perth was as follows:
· Rotary Blending & Splitting (12x1kg, reserve)
· PPS - Head Assay Submission
· Assay - Head Assay (Ce, La, Nd, Pr, SiO(2), Y)
· 1kg Grind Establishment (P80 53μm assumed)
· Rougher Flotation (6 con, 1 Tail)
· PPS - Float Products
· Assay - Head Assay (Ce, La, Nd, Pr, SiO(2), and Y)
Results
The head grade and froth flotation improvement are shown in Figure A1.
FIGURE A1: HEAD ASSAY / IMPROVEMENT
ANALYTE ALS Adelaide ALS Perth Times Improvement
REE ME-MS81 HEAD GRADE REE COMP %
%
Ce (%) 0.045 0.05 1.6
La (%) 0.038 0.03 2.3
Nd (%) 0.021 0.02 2.0
Pr (%) 0.006 0.01 1.3
SiO2 (%) NT 64.3 -
Y (%) 0.009 0.01 1.1
Source: ALS
Overall main laboratory observations of note are:
· Slurry was highly viscous after ALS Perth added lime that changed the
target pH down to 9.5. The process was changed to soda ash in the second test.
· By end of float, ALS Perth saw froth instability, which indicates
what material wanted to float.
· There was a colour trend in the concentrate progressing through the
stages.
Figures A2 to A5 show cumulative recovery versus grade for the Ce, La, Nd, and
Pr components.
FIGURE A1: CERIUM CUMULATIVE GRADE / RECOVERY
Source: ALS
FIGURE A1: LANTHANUM CUMULATIVE GRADE / RECOVERY
Source: ALS
FIGURE A1: NEODYMIUM UMULATIVE GRADE / RECOVERY
Source: ALS
FIGURE A5: PRASEODYMIUM CUMULATIVE GRADE / RECOVERY
Source: ALS
FIGURE A6: FLOWTATION FLOWSHEET
Source: ALS
FIGURE A7: DRILLHOLE FG_003RC - 0 TO 20M COMPOSITE USED FOR ALS PERTH METALLURGICAL TESTING, 1M ANALYSIS (A-P)
Sample From To Length PGM-MS23 PGM-MS23 PGM-MS23 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81
Number
Au Pt Pd Ba Ce Cr Cs Dy Er Eu Ga Gd Hf Ho La Lu Nb Nd Pr
m m m ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm
CCZ04511 0 1 1 0.002 0.001 0.002 297 131 61 3.13 6.48 3.92 1.71 23.5 7.17 5.56 1.35 70 0.58 10.85 54.8 16.1
CCZ04512 1 2 1 0.006 0.0013 0.003 910 172.5 73 2.58 7.57 4.05 2.16 38.1 8.71 4.09 1.52 97.5 0.46 10.55 74.2 21
CCZ04513 2 3 1 0.004 0.0011 0.002 648 696 71 2.64 20.9 9.3 9.12 46.2 34.4 4.18 3.6 409 0.93 12.75 347 94.2
CCZ04514 3 4 1 0.002 0.0007 0.001 166.5 580 72 5.2 17.85 6.75 7.5 55.9 28.5 3.02 2.76 369 0.54 10.4 276 74.4
CCZ04515 4 5 1 0.002 0.0007 0.001 143 511 80 5.01 16.35 6.43 6.46 51.2 25.9 3.39 2.67 336 0.63 13.85 252 67.4
CCZ04516 5 6 1 0.001 0.0008 0.001 98.4 376 75 3.04 10.5 3.86 3.91 53.5 17.5 3.05 1.62 229 0.36 12.8 175.5 46.6
CCZ04517 6 7 1 <0.001 0.0008 0.001 91.9 480 76 3.89 13.75 4.51 5.55 54.5 22.4 3.37 2.03 293 0.47 11.9 221 59.8
CCZ04518 7 8 1 <0.001 0.0007 0.001 59.1 332 90 3.2 8.64 3.14 3.43 60.5 14.3 3.18 1.33 204 0.28 15.4 142.5 39.3
CCZ04519 8 9 1 <0.001 0.0007 0.001 87.2 422 88 5.13 12.5 5.17 4.67 53.4 19 2.97 2.05 258 0.6 12.55 184.5 49.7
CCZ04520 9 10 1 <0.001 0.0008 0.001 94.5 287 78 5.62 7.68 3.76 2.49 56.5 10.55 2.62 1.37 175 0.49 13.2 116.5 31.3
CCZ04521 10 11 1 0.001 0.0007 0.001 110.5 366 81 6.57 8.9 4.09 3.31 48.3 14.05 2.56 1.69 231 0.55 10.95 145.5 42.6
CCZ04522 11 12 1 <0.001 0.0007 0.001 118.5 384 90 6.47 12.3 6.33 3.66 58.3 16.7 2.95 2.2 258 0.92 13.1 158.5 43.4
CCZ04523 12 13 1 <0.001 0.0007 0.001 88.6 292 85 3.63 9.33 5.15 2.71 57.2 12.45 3.51 1.79 202 0.61 12.7 117 32.1
CCZ04524 13 14 1 <0.001 0.0007 0.001 98.8 318 81 5.38 12.6 5.77 4.14 56.9 17.65 2.9 2.28 233 0.68 13.15 145.5 38.3
CCZ04525 14 15 1 <0.001 0.0009 0.001 45.7 486 91 4.58 17.9 6.78 5.7 63 28.4 3.06 2.93 341 0.61 12.45 222 59.1
CCZ04526 15 16 1 <0.001 0.0008 0.001 69.4 577 71 9.24 29 13.5 7.19 61.2 38.1 3.58 5.31 427 1.5 11.4 266 68.9
CCZ04527 16 17 1 0.001 0.0025 0.002 53.4 453 67 5.76 23.3 11.35 5.34 47.1 28 4.04 4.32 322 1.29 10.1 195 50.9
CCZ04528 17 18 1 0.003 0.0017 0.002 118 698 53 17.75 30.3 14.65 7.91 48.2 40.5 1.46 5.72 466 1.5 5.57 303 81.5
CCZ04529 18 19 1 0.045 0.002 0.002 109 774 54 6.11 42.4 16.05 12.35 40.3 60.8 1.61 6.9 644 1.36 6.51 425 106.5
CCZ04530 19 20 1 0.005 0.0011 0.001 193 661 60 2.69 104.5 69.3 15.6 25.8 100 2.98 23.8 597 8.34 7 403 94.2
Average 180.0 449.8 74.9 5.4 20.6 10.2 5.7 50.0 27.3 3.2 3.9 308.1 1.1 11.4 211.2 55.9
Source: ALS Adelaide methods ME-MS81 and PGM-MS23 used. Drillhole FG_003RC
drilled October 2022.
FIGURE A7: DRILLHOLE FG_003RC - 0 TO 20M COMPOSITE USED FOR ALS PERTH METALLURGICAL TESTING, 1M ANALYSIS (CONT)
Sample From To Length ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81
Number
Rb Sc Sm Sn Sr Ta Tb Th Ti Tm U V W Y Yb Zr
m m m ppm ppm ppm ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppm ppm ppm
CCZ04511 0 1 1 67.5 16.4 10.3 3.2 128 0.9 1.18 12.85 0.49 0.59 4.02 190 3.1 37 3.69 223
CCZ04512 1 2 1 51.2 20 12.35 2.4 180 0.8 1.28 13.65 0.41 0.55 7.54 247 4 35.3 3.39 134
CCZ04513 2 3 1 51.7 19.4 52.8 3.2 126 1 4.53 14.55 0.38 1.18 15.65 191 4.4 76.9 7.01 137
CCZ04514 3 4 1 92.2 37.5 41.8 3.5 129.5 1 3.79 16.3 0.33 0.84 13.85 171 2.8 50.3 5.02 109
CCZ04515 4 5 1 89.1 27.5 38.7 4.3 109.5 1.2 3.52 14.95 0.4 0.78 12.5 178 2.8 53.6 5.09 110
CCZ04516 5 6 1 51.2 14.7 25.9 3.5 91.3 1.1 2.28 16.25 0.38 0.55 7.46 129 3.7 30.9 2.88 100
CCZ04517 6 7 1 78.9 14.7 33.2 2.6 99.1 1 2.98 16.35 0.34 0.57 9.41 106 4.3 35.8 3.23 110
CCZ04518 7 8 1 79.8 11.6 22.6 3.2 101 1.2 1.88 18.25 0.38 0.38 7.65 102 6.3 25.5 2.31 107
CCZ04519 8 9 1 121 16.7 29 3.6 100 1.2 2.58 14.9 0.35 0.71 10.7 140 3 43.1 4.57 99
CCZ04520 9 10 1 160.5 19.6 16.3 3.5 84.7 1.1 1.5 14.3 0.32 0.55 8.74 150 2.2 28.2 4.08 87
CCZ04521 10 11 1 196 20.4 21.6 4.1 89.8 0.9 1.96 14.5 0.31 0.59 12.1 149 1.7 33.6 3.97 87
CCZ04522 11 12 1 171.5 20.2 24 3.7 117 1.1 2.28 19.6 0.34 0.96 15.85 149 3.5 50.9 6.62 99
CCZ04523 12 13 1 108.5 21.4 16.55 3.1 98.9 1.1 1.79 17.65 0.34 0.73 11.2 101 6.3 38.4 4.72 116
CCZ04524 13 14 1 131 20.4 22.3 5 103.5 1 2.28 17.3 0.33 0.79 12.5 136 4 49 4.78 97
CCZ04525 14 15 1 98.8 15.7 35.2 4.3 88.2 1.1 3.64 18.45 0.36 0.81 14.2 170 3.5 57 5 95
CCZ04526 15 16 1 143.5 19.2 41.5 4.3 81.2 1 5.56 18.25 0.31 1.78 20.7 184 2.7 115.5 11.75 113
CCZ04527 16 17 1 84.4 17.6 30.9 3.5 64.9 0.9 4.24 12.7 0.27 1.54 19.1 147 3.6 95.8 9.92 142
CCZ04528 17 18 1 139.5 17.8 47 3.8 51.4 0.4 5.61 6.91 0.15 1.98 38.1 498 4.2 137 12.55 53
CCZ04529 18 19 1 52 38.5 66 5.7 110 0.4 8.47 4.76 0.74 1.94 73.4 580 3 128 11.6 50
CCZ04530 19 20 1 32.7 41.9 72.2 1.5 146 0.4 16 1.57 1.11 9.13 48.7 442 1.1 722 57.8 94
Average 100.1 21.6 33.0 3.6 105.0 0.9 3.9 14.2 0.4 1.3 18.2 208.0 3.5 92.2 8.5 108.1
Source: ALS Adelaide methods ME-MS81 and PGM-MS23 used. Drillhole FG_003RC
drilled October 2022.
APPENDIX C: REE RESULTS / TREO CONVERSION FACTOR
FIGURE B1: FENCE GOSSAN SURFACE SAMPLING - ALS METHOD ME-MS81 LABORATORY
RESULTS
HoleID Sampid Easting Northing from to thickness Th U Ce La Y Dy Er Eu Gd Ho Lu Nd Pr Sm Tb Tm Yb TREO (ppm) TREO-Ce (ppm) LREO (ppm) HREO (ppm) CREO % MREO % MREO_%
FG_SM_T12 CCZ05627 574597.0 6454393.0 0 0.3 0.3 16.0 2.5 113.5 53.6 41.3 7.49 4.33 1.6 8.57 1.49 0.54 49.3 12.95 9.54 1.31 0.59 4.04 373.4 233.9 286.5 86.9 0.33 0.28 27.9
FG_SM_T13 CCZ05628 574601.0 6454194.0 0 0.3 0.3 12.9 2.1 77.7 37.2 36.6 5.95 3.91 1.33 6.33 1.36 0.54 34.9 8.87 6.74 1.03 0.58 3.7 273.2 177.7 198.3 74.9 0.35 0.27 27.3
FG_SM_T14 CCZ05629 574600.0 6453990.0 0 0.3 0.3 14.9 2.2 88.6 43.1 31.1 5.25 3.28 1.11 6.03 1.12 0.46 37.7 10.15 7.22 0.95 0.46 3.05 288.4 179.6 224.0 64.4 0.32 0.27 27.3
FG_SM_T15 CCZ05630 574600.0 6453791.0 0 0.3 0.3 12.8 1.8 73.9 36.2 30.4 5.16 3.17 1.21 6.01 1.09 0.4 33.4 8.87 6.81 0.91 0.48 3.01 254.0 163.3 190.8 63.2 0.34 0.28 28.1
FG_SM_T16 CCZ05631 574599.0 6453588.0 0 0.3 0.3 13.8 1.9 83.5 39.9 32.1 5.65 3.17 1.31 6.31 1.2 0.41 37.7 9.93 7.66 0.99 0.45 2.94 280.8 178.2 214.2 66.5 0.33 0.28 28.4
FG_SM_T17 CCZ05632 574602.0 6453389.0 0 0.3 0.3 14.4 2.0 85.2 41.1 33.3 5.52 3.58 1.19 6.08 1.19 0.55 37.4 9.9 6.89 0.92 0.55 3.7 285.5 180.8 216.4 69.0 0.33 0.27 27.3
FG_SM_T18 CCZ05633 574598.0 6453194.0 0 0.3 0.3 12.1 1.8 84.4 35.7 29 4.93 3.07 1.22 5.79 1.09 0.41 32.2 8.45 6.07 0.92 0.46 2.89 261.0 157.4 200.4 60.7 0.32 0.26 26.1
FG_SM_T19 CCZ05634 574601.0 6452990.0 0 0.3 0.3 13.7 1.9 84.5 41.5 34.6 5.92 3.95 1.34 6.61 1.24 0.48 38.1 9.89 7.45 1.01 0.55 3.64 289.8 186.0 217.5 72.3 0.34 0.28 27.8
FG_SM_T20 CCZ05635 574600.0 6452790.0 0 0.3 0.3 18.3 2.6 104.5 51.5 36.1 6.3 3.94 1.32 7.3 1.31 0.46 46.2 12 9.12 1.06 0.53 3.63 343.3 214.9 267.7 75.5 0.32 0.28 27.9
FG_SM_U12 CCZ05636 574800.0 6454396.0 0 0.3 0.3 17.9 2.4 108.5 51.6 37.6 6.73 3.74 1.49 7.61 1.33 0.51 46.7 12.8 9.28 1.15 0.58 3.54 352.9 219.6 274.5 78.4 0.32 0.28 27.9
FG_SM_U13 CCZ05637 574799.0 6454196.0 0 0.3 0.3 16.6 2.3 98.9 48.7 49.7 8.11 5.28 1.5 9.26 1.82 0.75 46.1 11.95 9.47 1.45 0.8 5.15 360.1 238.6 257.8 102.3 0.36 0.28 28.0
FG_SM_U14 CCZ05638 574802.0 6453995.0 0 0.3 0.3 12.5 2.0 75.1 37.5 42.2 6.24 4.31 1.12 6.31 1.49 0.59 33.9 8.91 6.78 0.99 0.71 4.43 278.0 185.8 194.4 83.6 0.37 0.27 26.5
FG_SM_U15 CCZ05639 574800.0 6453795.0 0 0.3 0.3 14.8 2.3 79.5 37.4 42 6.89 4.58 1.24 6.76 1.57 0.61 35.5 9.28 7.26 1.15 0.71 4.48 288.0 190.4 202.6 85.5 0.37 0.27 27.1
FG_SM_U16 CCZ05640 574803.0 6453599.0 0 0.3 0.3 14.5 2.1 84.8 42.7 37.9 6.2 3.87 1.33 6.34 1.3 0.56 37.9 10.05 7.54 1.06 0.58 3.72 296.1 192.0 219.3 76.8 0.35 0.27 27.3
FG_SM_U17 CCZ05641 574800.0 6453399.0 0 0.3 0.3 14.5 2.2 88.7 44.5 32.5 5.49 3.37 1.23 6.04 1.17 0.49 38.8 10.6 7.47 0.98 0.52 3.1 294.9 185.9 227.9 67.0 0.32 0.28 27.5
FG_SM_U18 CCZ05642 574800.0 6453199.0 0 0.3 0.3 13.4 2.1 78.3 38.8 32.3 5.35 3.28 1.2 5.69 1.09 0.46 35.1 9.27 7.11 0.86 0.45 3.09 267.7 171.6 202.1 65.7 0.34 0.28 27.7
FG_SM_U19 CCZ05643 574799.0 6453000.0 0 0.3 0.3 17.1 2.3 104.5 51 38.2 6.25 3.78 1.44 7.53 1.33 0.6 45.3 12.3 9.02 1.11 0.61 3.63 345.0 216.7 266.3 78.7 0.32 0.28 27.6
FG_SM_U20 CCZ05644 574801.0 6452798.0 0 0.3 0.3 18.4 2.9 105.5 50.5 38.3 6.25 3.97 1.39 7.23 1.35 0.57 45.7 12.2 8.94 1.1 0.57 3.64 345.8 216.2 267.2 78.6 0.32 0.28 27.5
FG_SM_V12 CCZ05645 574999.0 6454394.0 0 0.3 0.3 12.1 1.6 71.3 36.2 27.8 4.74 2.82 1.11 5.23 0.93 0.41 31.8 8.52 6.49 0.83 0.42 2.58 242.2 154.6 185.0 57.2 0.33 0.28 27.8
FG_SM_V13 CCZ05646 575001.0 6454190.0 0 0.3 0.3 15.0 2.2 105 50.3 44.2 7.19 4.65 1.25 7.83 1.55 0.67 45.2 12.1 8.95 1.24 0.66 4.09 355.3 226.3 265.7 89.6 0.34 0.27 27.1
FG_SM_V14 CCZ05647 574999.0 6453995.0 0 0.3 0.3 12.7 1.9 72.8 37.3 38.3 6.21 3.82 1.32 6.08 1.32 0.56 32.9 9.01 6.89 0.99 0.57 3.78 267.4 177.9 190.4 76.9 0.36 0.27 27.1
FG_SM_V15 CCZ05648 574999.0 6453792.0 0 0.3 0.3 15.8 3.3 130.5 64.6 63 10.85 6.35 2.31 11.9 2.23 0.88 62 16.3 13.05 1.84 0.97 5.99 473.0 312.7 343.2 129.8 0.36 0.29 28.6
FG_SM_V16 CCZ05649 575004.0 6453591.0 0 0.3 0.3 16.2 2.7 100 49.9 39.1 6.6 4.1 1.33 7.36 1.37 0.62 43.5 11.6 8.71 1.1 0.61 3.81 336.8 213.9 256.2 80.5 0.33 0.27 27.4
FG_SM_V17 CCZ05650 575000.0 6453393.0 0 0.3 0.3 14.5 2.3 88.5 45.1 36.8 6.15 3.83 1.35 6.56 1.32 0.55 40.8 10.6 7.87 1.02 0.55 3.52 306.4 197.7 231.1 75.3 0.34 0.28 27.9
FG_SM_V18 CCZ05651 575001.0 6453195.0 0 0.3 0.3 14.5 2.4 80 40 31.4 5.28 3.21 1.23 5.69 1.09 0.46 34.6 9.37 7.09 0.9 0.49 3.18 269.7 171.4 205.1 64.6 0.33 0.27 27.3
FG_SM_V19 CCZ05652 574999.0 6452991.0 0 0.3 0.3 13.1 2.2 73.9 36.6 31.2 5.23 3.23 1.04 5.29 1.08 0.49 32 8.7 6.42 0.88 0.49 3.14 252.6 161.8 189.0 63.6 0.34 0.27 27.1
FG_SM_V20 CCZ05653 575001.0 6452793.0 0 0.3 0.3 15.2 2.2 82.2 41.6 34.3 5.31 3.46 1.07 5.99 1.13 0.49 36.5 9.89 7.19 0.86 0.5 3.22 281.5 180.5 212.6 68.9 0.34 0.27 27.3
FG_SM_W12 CCZ05654 575202.0 6454400.0 0 0.3 0.3 16.3 2.3 93.7 45.8 39.4 6.58 4.06 1.37 7.54 1.43 0.57 42.3 11.35 8.53 1.16 0.61 3.97 323.1 208.0 241.8 81.4 0.34 0.28 28.0
FG_SM_W13 CCZ05655 575203.0 6454197.0 0 0.3 0.3 19.5 2.4 91.8 43.7 41.6 6.6 4.21 1.24 7.31 1.43 0.63 39.8 10.8 8.39 1.1 0.64 4.12 317.4 204.6 233.2 84.1 0.35 0.27 27.3
FG_SM_W14 CCZ05656 575203.0 6453997.0 0 0.3 0.3 13.2 2.3 93.2 46.2 40 6.6 4.11 1.41 7.1 1.44 0.58 41.3 11.05 8.3 1.1 0.58 3.75 321.2 206.8 239.8 81.4 0.34 0.27 27.5
FG_SM_W15 CCZ05657 575200.0 6453793.0 0 0.3 0.3 12.5 2.4 106 50.7 49 8.36 4.86 1.79 9.19 1.71 0.71 47.7 12.05 10.15 1.45 0.73 4.46 372.1 241.9 271.6 100.4 0.35 0.28 27.9
FG_SM_W16 CCZ05658 575203.0 6453593.0 0 0.3 0.3 15.8 2.7 102.5 52.5 42.6 6.76 4.16 1.46 7.46 1.4 0.67 44.8 12.2 9.06 1.2 0.67 4.17 351.2 225.3 265.0 86.2 0.33 0.27 27.1
FG_SM_W17 CCZ05659 575198.0 6453396.0 0 0.3 0.3 14.6 2.1 90.2 47.8 30.3 5.44 3.08 1.5 6.4 1.08 0.43 42.7 11.85 8.4 0.94 0.47 2.71 304.5 193.7 240.7 63.8 0.32 0.29 29.1
FG_SM_W18 CCZ05660 575201.0 6453200.0 0 0.3 0.3 15.7 3.0 98.4 52.8 38.7 6.24 4 1.44 7.08 1.36 0.58 43.3 11.8 8.71 1.06 0.61 3.95 337.0 216.2 257.7 79.4 0.33 0.27 27.1
FG_SM_W19 CCZ05661 575204.0 6452996.0 0 0.3 0.3 12.4 1.9 69.2 35.5 34 5.23 3.68 1.21 5.16 1.15 0.61 32.4 8.49 6.17 0.81 0.59 3.75 250.5 165.5 181.8 68.6 0.36 0.27 27.2
FG_SM_W20 CCZ05662 575202.0 6452795.0 0 0.3 0.3 13.7 2.4 58.2 32 28.9 4.49 3.02 0.95 4.72 0.96 0.47 26.4 7.33 5.19 0.7 0.45 3.13 213.1 141.6 154.7 58.4 0.35 0.27 26.8
FG_SM_X12 CCZ05663 575399.0 6454396.0 0 0.3 0.3 19.3 2.3 109 52.7 54.8 8.73 6.03 1.34 8.22 1.9 0.84 45.7 12.4 9.23 1.34 0.92 5.47 384.2 250.3 274.7 109.5 0.35 0.26 26.0
FG_SM_X13 CCZ05664 575400.0 6454192.0 0 0.3 0.3 15.4 3.0 99 48 51.2 8.67 5.28 1.3 8.88 1.83 0.74 44.1 11.7 9.48 1.51 0.81 4.8 358.3 236.7 254.5 103.9 0.36 0.27 27.5
FG_SM_X14 CCZ05665 575402.0 6453996.0 0 0.3 0.3 20.7 3.3 153 82.7 56.1 9.61 5.75 1.85 9.91 2.06 0.86 62.8 17.2 12.25 1.62 0.83 5.35 507.9 319.9 393.2 114.7 0.31 0.26 26.1
FG_SM_X15 CCZ05666 575400.0 6453795.0 0 0.3 0.3 15.6 2.6 98.8 50.4 34.2 5.79 3.24 1.36 6.92 1.18 0.47 42.2 11.35 8.32 1 0.49 3.09 323.5 202.2 253.1 70.5 0.32 0.27 27.3
FG_SM_X16 CCZ05667 575399.0 6453591.0 0 0.3 0.3 15.1 2.8 112.5 59.4 42.4 7.17 4.39 1.72 8.12 1.48 0.62 49.2 13.3 9.16 1.21 0.66 4.07 379.6 241.4 291.9 87.7 0.32 0.27 27.2
FG_SM_X17 CCZ05668 575402.0 6453394.0 0 0.3 0.3 13.7 2.3 98.5 49.7 32.3 5.61 3.28 1.55 6.79 1.16 0.49 43.3 11.75 8.75 1.01 0.47 3.27 322.3 201.3 254.1 68.2 0.31 0.28 28.0
FG_SM_X18 CCZ05669 575404.0 6453192.0 0 0.3 0.3 13.9 2.5 126.5 53.2 45.3 7.54 5 1.95 8.49 1.59 0.76 53.9 13.7 11 1.3 0.74 4.77 404.4 249.0 310.0 94.4 0.33 0.28 27.7
FG_SM_X19 CCZ05670 575398.0 6452993.0 0 0.3 0.3 17.1 2.7 106.5 50.9 37.6 6.32 3.96 1.52 7.16 1.28 0.56 44.9 12.25 8.79 1.07 0.54 3.71 345.6 214.8 267.9 77.7 0.32 0.27 27.2
FG_SM_X20 CCZ05671 575400.0 6452792.0 0 0.3 0.3 14.7 2.5 96.4 47.4 37.4 5.94 3.85 1.5 6.75 1.28 0.58 41.6 11.45 8.28 1.03 0.59 3.64 322.4 203.9 246.0 76.4 0.33 0.27 27.2
FG_SM_Y12 CCZ05672 575600.0 6454397.0 0 0.3 0.3 18.1 2.5 111.5 57.8 45.3 8.02 4.8 1.54 8.88 1.63 0.63 52.8 14.2 10.35 1.36 0.71 4.23 389.5 252.6 295.5 94.0 0.34 0.29 28.7
FG_SM_Y13 CCZ05673 575592.0 6454191.0 0 0.3 0.3 11.1 2.5 102 51.6 42.3 7.62 4.41 1.46 8.1 1.51 0.65 46.3 11.95 9.22 1.26 0.69 4.13 352.9 227.6 264.9 88.0 0.34 0.28 28.0
FG_SM_Y14 CCZ05674 575600.0 6453999.0 0 0.3 0.3 18.3 2.9 125.5 63.1 50.9 8.5 5.34 1.58 8.97 1.79 0.83 52.2 14.55 10.6 1.46 0.78 4.88 422.8 268.6 318.9 103.8 0.33 0.27 26.6
FG_SM_Y15 CCZ05675 575599.0 6453797.0 0 0.3 0.3 14.3 2.7 112 59.1 41.9 6.45 4.12 1.5 7.47 1.36 0.62 49.2 13.3 9.14 1.18 0.62 3.87 375.4 237.8 290.9 84.4 0.32 0.27 27.0
FG_SM_Y16 CCZ05676 575600.0 6453598.0 0 0.3 0.3 16.2 2.6 100.5 52.4 29.2 4.77 2.82 1.26 5.89 0.98 0.4 43.1 12.1 8 0.89 0.45 2.73 319.4 195.9 259.1 60.3 0.30 0.27 27.4
FG_SM_Y17 CCZ05677 575600.0 6453400.0 0 0.3 0.3 12.7 2.2 77.4 40.6 35.4 5.79 3.5 1.33 6.34 1.18 0.49 36.2 9.73 7.52 0.96 0.53 3.45 277.4 182.3 205.4 72.0 0.35 0.28 28.0
FG_SM_Y18 CCZ05678 575598.0 6453200.0 0 0.3 0.3 17.8 2.8 107.5 53.5 36.4 6.05 3.51 1.59 7.03 1.28 0.51 47.6 12.55 8.92 1.08 0.55 3.43 350.8 218.7 275.8 75.0 0.32 0.28 27.7
FG_SM_Y19 CCZ05679 575600.0 6452995.0 0 0.3 0.3 18.4 2.8 105 55.9 40.4 6.74 3.94 1.53 7.72 1.38 0.6 49.9 13.7 9.87 1.14 0.63 3.8 363.6 234.6 280.7 82.9 0.33 0.29 28.7
FG_SM_Y20 CCZ05680 575598.0 6452799.0 0 0.3 0.3 19.3 2.8 115 56 37.4 6.46 3.52 1.33 7.56 1.26 0.52 51.4 13.65 9.9 1.14 0.55 3.27 371.8 230.5 294.9 76.9 0.32 0.28 28.3
FG_SM_Z12 CCZ05681 575795.0 6454397.0 0 0.3 0.3 17.7 2.8 126.5 65.3 61.7 9.72 5.93 1.61 10.45 2.09 0.82 58.5 15.85 11.7 1.71 0.88 5.55 455.8 300.4 332.9 122.9 0.35 0.28 27.7
FG_SM_Z13 CCZ05682 575791.0 6454200.0 0 0.3 0.3 14.1 2.8 113.5 58.9 52.5 8.7 5.3 1.83 9.14 1.89 0.75 52.3 13.75 10.15 1.5 0.82 4.83 404.5 265.1 297.9 106.6 0.35 0.28 27.6
FG_SM_Z14 CCZ05683 575806.0 6453995.0 0 0.3 0.3 14.3 2.0 85.7 43.9 36.2 6.8 3.96 1.48 6.8 1.34 0.5 41.2 11 8.07 1.16 0.59 3.6 303.6 198.3 227.5 76.1 0.35 0.29 28.9
FG_SM_Z15 CCZ05684 575799.0 6453795.0 0 0.3 0.3 13.1 2.9 129 66.4 32.1 5.82 3.12 1.54 7.34 1.11 0.4 51.4 15.1 9.37 1.12 0.43 2.8 393.4 234.9 325.4 68.0 0.28 0.27 26.8
FG_SM_Z16 CCZ05685 575799.0 6453594.0 0 0.3 0.3 12.9 2.5 78.7 39.8 30.8 5.46 3.33 1.33 5.92 1.2 0.46 36.5 9.66 7.18 0.96 0.48 3.1 270.6 173.9 205.9 64.7 0.33 0.28 28.4
FG_SM_Z17 CCZ05686 575797.0 6453396.0 0 0.3 0.3 12.4 2.3 83.3 45.3 44.8 6.7 4.24 1.61 7.39 1.49 0.62 41.2 10.75 8.02 1.18 0.61 3.91 314.6 212.2 225.8 88.8 0.37 0.28 28.0
FG_SM_Z18 CCZ05687 575798.0 6453193.0 0 0.3 0.3 17.2 2.7 111.5 54 49 7.87 5 1.77 8.66 1.69 0.72 48.5 13 9.51 1.33 0.76 4.85 383.3 246.4 283.6 99.7 0.34 0.27 27.1
FG_SM_Z19 CCZ05688 575802.0 6452992.0 0 0.3 0.3 18.1 3.0 108 55.1 45.8 7.17 4.48 1.29 7.39 1.53 0.65 47.6 13.1 8.86 1.26 0.72 4.4 370.2 237.6 278.9 91.3 0.34 0.27 27.0
FG_SM_Z20 CCZ05689 575800.0 6452800.0 0 0.3 0.3 17.3 2.7 118.5 60.5 35.5 6 3.5 1.42 7.06 1.2 0.49 50.2 14.25 9.27 1.07 0.53 3.32 376.4 230.8 303.0 73.3 0.30 0.27 27.3
FG_SM_AA12 CCZ05690 576000.0 6454400.0 0 0.3 0.3 13.0 2.0 86.6 44.2 42.2 6.77 4.39 1.26 7.2 1.49 0.59 40.6 10.5 8.41 1.22 0.64 3.95 313.2 206.8 228.0 85.2 0.36 0.28 27.9
FG_SM_AA13 CCZ05691 576002.0 6454198.0 0 0.3 0.3 13.7 2.0 100.5 54.3 41.8 7.15 4.24 1.64 7.97 1.53 0.59 49.3 13.35 9.68 1.32 0.63 3.93 358.4 234.9 272.0 86.4 0.34 0.29 29.0
FG_SM_AA14 CCZ05692 575997.0 6453998.0 0 0.3 0.3 15.0 2.9 107.5 53.9 36.6 6.55 4.24 1.34 7.24 1.42 0.55 46.4 12.65 9.51 1.18 0.56 4.08 353.4 221.3 275.7 77.7 0.31 0.28 27.6
FG_SM_AA15 CCZ05693 575999.0 6453799.0 0 0.3 0.3 10.4 3.3 130.5 65.2 39.8 7.79 4.09 1.94 8.2 1.51 0.47 57.6 15.4 9.7 1.21 0.66 3.95 418.6 258.3 333.8 84.8 0.31 0.28 27.9
FG_SM_AA16 CCZ05694 576003.0 6453601.0 0 0.3 0.3 13.7 2.1 85 44.6 30.6 5.37 3.05 1.38 6.23 1.06 0.44 38.5 10.5 7.5 0.93 0.46 2.89 286.9 182.5 223.0 63.9 0.32 0.28 28.1
FG_SM_AA17 CCZ05695 575999.0 6453398.0 0 0.3 0.3 12.0 2.1 72.6 38 29.7 5.09 2.99 1.14 5.74 1.04 0.46 33.4 8.92 6.18 0.89 0.44 2.79 252.0 162.8 190.7 61.4 0.34 0.28 27.9
FG_SM_AA18 CCZ05696 575999.0 6453197.0 0 0.3 0.3 15.3 2.6 92.9 48.1 40.7 6.28 3.88 1.33 6.74 1.32 0.63 42.6 11.5 8.04 1.12 0.63 4.03 324.9 210.8 243.4 81.5 0.34 0.27 27.5
FG_SM_AA19 CCZ05697 576006.0 6453003.0 0 0.3 0.3 17.3 2.8 106.5 54.2 33.3 5.53 3.12 1.39 7.01 1.13 0.45 46.4 12.75 8.77 1.07 0.49 2.93 342.9 212.1 274.1 68.9 0.31 0.28 27.8
FG_SM_AA20 CCZ05698 576002.0 6452797.0 0 0.3 0.3 13.4 2.2 84.2 44.4 28.4 4.58 2.85 1.46 5.98 0.94 0.41 38.6 10.65 7.17 0.9 0.42 2.63 280.9 177.5 221.7 59.2 0.32 0.28 28.3
FG_SM_AB12 CCZ05699 576200.0 6454398.0 0 0.3 0.3 17.9 2.6 107.5 54 45.8 7.49 4.82 1.27 8.23 1.52 0.63 49 13.4 9.79 1.36 0.72 4.47 373.3 241.2 280.1 93.2 0.34 0.28 28.0
FG_SM_AB13 CCZ05700 576202.0 6454197.0 0 0.3 0.3 14.8 2.1 91.3 48 37.5 6.21 3.66 1.42 7.19 1.33 0.54 42.5 11.3 8.53 1.1 0.56 3.45 318.4 206.3 241.6 76.9 0.34 0.28 28.2
FG_SM_AB14 CCZ05701 576201.0 6453998.0 0 0.3 0.3 13.8 2.4 105.5 57.5 37.7 6.32 3.64 1.68 7.73 1.29 0.48 48.3 13.15 9.83 1.18 0.53 3.27 358.5 228.9 280.7 77.9 0.32 0.28 28.2
FG_SM_AB15 CCZ05702 576201.0 6453797.0 0 0.3 0.3 11.2 3.4 105 62.5 39.9 6.13 3.61 1.51 7.17 1.28 0.54 45.7 12.75 8.12 1.1 0.54 3.39 360.1 231.1 280.4 79.7 0.32 0.26 26.3
FG_SM_AB16 CCZ05703 576200.0 6453598.0 0 0.3 0.3 14.0 2.5 87.8 45.4 27.4 4.54 2.82 1.2 5.8 0.96 0.4 39 10.7 6.88 0.9 0.45 2.7 285.0 177.1 227.5 57.5 0.31 0.28 27.8
FG_SM_AB17 CCZ05704 576199.0 6453396.0 0 0.3 0.3 12.5 2.2 71.6 37.4 32 5.21 3.4 1.12 5.66 1.09 0.44 33.6 8.73 6.47 0.87 0.46 3.05 254.2 166.2 189.1 65.1 0.35 0.28 27.8
FG_SM_AB18 CCZ05705 576200.0 6453195.0 0 0.3 0.3 18.8 3.2 117.5 60.1 58.4 9.2 5.97 1.63 8.77 1.98 0.92 51.2 14.25 9.62 1.54 0.96 5.71 419.2 274.8 302.9 116.3 0.35 0.26 26.4
FG_SM_AB19 CCZ05706 576200.0 6452999.0 0 0.3 0.3 19.1 3.2 116 59.6 38 6.34 3.74 1.43 7.55 1.28 0.52 50.3 14.1 9.61 1.16 0.58 3.57 377.6 235.1 299.2 78.3 0.31 0.28 27.6
FG_SM_AB20 CCZ05707 576198.0 6452797.0 0 0.3 0.3 18.3 3.2 109.5 56.5 36.6 5.95 3.55 1.43 7.49 1.22 0.52 47.2 12.85 8.51 1.09 0.55 3.5 356.8 222.3 281.2 75.5 0.31 0.27 27.2
FG_SM_AC12 CCZ05708 576403.0 6454399.0 0 0.3 0.3 14.6 2.0 78.2 40.5 34.7 5.59 3.5 1.21 5.74 1.18 0.5 36.2 9.62 7.25 0.95 0.56 3.4 275.9 179.8 205.8 70.0 0.35 0.28 27.7
FG_SM_AC13 CCZ05709 576402.0 6454197.0 0 0.3 0.3 11.2 1.8 89.1 46 31 5.27 3.16 1.63 6.34 1.08 0.43 40.6 11.25 8.08 0.99 0.5 2.87 298.7 189.2 233.7 65.0 0.32 0.28 28.4
FG_SM_AC14 CCZ05710 576402.0 6453998.0 0 0.3 0.3 14.2 2.2 86.4 44.4 30.5 5.04 2.81 1.28 5.56 1.07 0.44 38.9 10.45 7.4 0.88 0.42 2.72 286.7 180.6 224.8 62.0 0.32 0.28 27.8
FG_SM_AC15 CCZ05711 576400.0 6453794.0 0 0.3 0.3 11.8 3.9 143.5 72.2 43.3 7.85 4.42 1.94 9.23 1.61 0.6 60.7 15.65 11.2 1.38 0.63 4.12 455.1 278.9 363.6 91.5 0.30 0.27 27.2
FG_SM_AC16 CCZ05712 576403.0 6453599.0 0 0.3 0.3 16.2 2.6 113 55.1 32.2 5.92 3.02 1.45 6.86 1.17 0.44 48.9 13 8.85 0.99 0.44 2.95 354.0 215.2 286.4 67.6 0.30 0.28 27.9
FG_SM_AC17 CCZ05713 576402.0 6453397.0 0 0.3 0.3 15.8 2.3 101 50.8 36.2 6.39 3.55 1.56 7.35 1.33 0.48 46.8 12.2 8.94 1.09 0.51 3.34 338.7 214.7 263.3 75.4 0.33 0.29 28.6
FG_SM_AC18 CCZ05714 576401.0 6453199.0 0 0.3 0.3 15.7 2.7 102 50.8 44.5 7.27 4.54 1.28 7.67 1.57 0.67 46.5 11.85 8.65 1.16 0.65 4.42 353.5 228.2 263.5 90.1 0.34 0.27 27.5
FG_SM_AC19 CCZ05715 576402.0 6452999.0 0 0.3 0.3 18.9 3.1 116.5 56.5 32.5 6.02 3.33 1.42 7.73 1.2 0.44 51.5 13.9 9.53 1.11 0.44 3.09 367.0 223.9 297.3 69.7 0.30 0.29 28.6
FG_SM_AC20 CCZ05716 576398.0 6452800.0 0 0.3 0.3 20.2 3.7 229 115 38.4 7.22 3.71 2.02 9.82 1.41 0.5 89.7 25.5 14.7 1.4 0.49 3.34 651.8 370.5 568.7 83.1 0.25 0.27 26.7
FG_SM_AD12 CCZ05717 576600.0 6454399.0 0 0.3 0.3 13.3 2.4 93.4 45.4 33.6 5.62 3.4 1.24 6.4 1.25 0.48 40.3 10.5 6.98 0.96 0.5 3.37 305.1 190.4 235.8 69.3 0.32 0.27 27.1
FG_SM_AD13 CCZ05718 576602.0 6454197.0 0 0.3 0.3 11.7 2.0 87.8 44.2 37.8 7.21 4.01 1.62 7.6 1.36 0.48 44.6 11.75 8.29 1.22 0.58 3.58 315.3 207.4 235.5 79.8 0.35 0.30 29.9
FG_SM_AD14 CCZ05719 576601.0 6453992.0 0 0.3 0.3 14.1 2.3 89.4 46 37.3 6.8 4.11 1.7 6.92 1.4 0.57 45 11.7 8.21 1.12 0.59 3.97 318.5 208.7 239.9 78.6 0.35 0.29 29.3
FG_SM_AD15 CCZ05720 576602.0 6453794.0 0 0.3 0.3 12.3 3.9 93 52.4 28.1 5.2 3.25 1.34 6.16 1.06 0.39 40.9 11.2 7.4 0.93 0.46 2.88 306.1 191.9 245.5 60.6 0.30 0.27 27.4
FG_SM_AD16 CCZ05721 576601.0 6453596.0 0 0.3 0.3 15.0 2.7 93 45.2 32.1 6.16 3.42 1.46 6.65 1.26 0.47 43.6 11.5 7.9 1.06 0.48 3.09 309.6 195.3 241.2 68.4 0.33 0.29 29.0
FG_SM_AD17 CCZ05722 576600.0 6453393.0 0 0.3 0.3 17.1 2.9 114 53.6 40.4 7.1 4.41 1.6 7.79 1.38 0.59 50.8 13.4 9.16 1.17 0.59 3.78 372.9 232.9 289.0 83.9 0.33 0.28 28.0
FG_SM_AD18 CCZ05723 576602.0 6453193.0 0 0.3 0.3 20.1 3.3 124.5 61.3 42.1 7.57 4.49 1.58 8.14 1.46 0.61 56.6 15.75 10.35 1.38 0.6 3.94 409.5 256.6 321.9 87.7 0.32 0.29 28.5
FG_SM_AD19 CCZ05724 576599.0 6452995.0 0 0.3 0.3 21.3 3.8 145 70.6 40.8 7.01 3.87 1.61 8.29 1.41 0.52 62.1 16.6 11.4 1.24 0.57 3.85 451.0 272.9 366.6 84.4 0.30 0.28 27.7
FG_SM_AD20 CCZ05725 576600.0 6452793.0 0 0.3 0.3 20.7 3.8 153.5 75.7 41 7.44 4.05 1.77 8.8 1.48 0.59 65.1 17.5 11.25 1.32 0.57 3.67 473.6 285.1 387.5 86.2 0.30 0.28 27.5
FG_SM_AE12 CCZ05726 576799.0 6454395.0 0 0.3 0.3 13.5 1.8 78.4 39.5 30.4 5.28 3.17 1.22 6.08 1.09 0.44 38.1 9.65 6.89 0.87 0.44 3 270.1 173.8 206.7 63.4 0.34 0.29 28.9
FG_SM_AE13 CCZ05727 576803.0 6454195.0 0 0.3 0.3 15.4 2.3 104 51.4 37.5 6.69 3.86 1.52 7.17 1.38 0.51 47.9 12.55 9.12 1.14 0.54 3.49 347.5 219.7 269.6 77.8 0.33 0.28 28.5
FG_SM_AE14 CCZ05728 576803.0 6453996.0 0 0.3 0.3 15.1 2.4 101.5 51.5 34.7 6.15 3.59 1.4 7.13 1.27 0.54 46.3 11.9 8.5 1.09 0.51 3.35 336.1 211.5 263.3 72.8 0.32 0.28 28.2
FG_SM_AE15 CCZ05729 576802.0 6453796.0 0 0.3 0.3 12.4 2.2 78.4 40.3 28.3 4.86 2.88 1.16 5.53 1.01 0.39 35.6 9.42 6.97 0.84 0.42 2.64 263.2 166.9 204.6 58.6 0.32 0.28 28.1
FG_SM_AE16 CCZ05730 576800.0 6453594.0 0 0.3 0.3 14.1 2.7 120 55.6 48.3 7.72 4.79 1.66 7.99 1.76 0.74 52 13.45 9.33 1.3 0.73 4.79 397.8 250.4 300.3 97.5 0.34 0.27 27.0
FG_SM_AE17 CCZ05731 576803.0 6453397.0 0 0.3 0.3 15.1 2.6 119.5 55.8 35.6 6.22 3.66 1.52 7.33 1.29 0.46 52.1 13.55 9.36 1.1 0.49 3.29 374.6 227.8 300.2 74.3 0.31 0.28 28.0
FG_SM_AE18 CCZ05732 576802.0 6453196.0 0 0.3 0.3 22.1 3.4 147 69.4 40.2 7.46 3.9 1.6 8.73 1.42 0.53 62.3 16.6 11.25 1.28 0.56 3.7 452.3 271.7 367.7 84.6 0.30 0.28 27.8
FG_SM_AE19 CCZ05733 576805.0 6453000.0 0 0.3 0.3 20.1 3.5 167 77.4 37.6 6.71 3.65 1.68 8.65 1.4 0.5 68 18.4 11.75 1.26 0.55 3.6 491.0 285.9 411.1 79.9 0.28 0.27 27.4
FG_SM_AE20 CCZ05734 576803.0 6452797.0 0 0.3 0.3 20.9 3.7 134 64.4 48.5 8 4.98 1.55 8.49 1.66 0.76 58.8 15.4 10.15 1.26 0.79 5.08 438.1 273.5 339.1 99.0 0.33 0.27 27.3
FG_SM_AF12 CCZ05735 577004.0 6454394.0 0 0.3 0.3 15.0 2.1 88.3 42.7 38 6.3 3.83 1.2 6.62 1.36 0.53 40.4 10.45 7.3 1.02 0.57 3.83 304.0 195.6 226.8 77.3 0.35 0.28 27.7
FG_SM_AF13 CCZ05736 577002.0 6454198.0 0 0.3 0.3 16.7 2.8 138 64.4 42.6 7.64 4.23 1.67 8.67 1.56 0.66 60.7 16.05 10.9 1.32 0.63 3.9 436.8 267.2 347.9 88.9 0.31 0.28 28.2
FG_SM_AF14 CCZ05737 577001.0 6453993.0 0 0.3 0.3 15.2 2.9 105 51.5 29.8 5.56 3.04 1.26 6.42 1.15 0.41 44.9 11.95 7.82 0.97 0.45 2.77 328.4 199.4 265.3 63.2 0.30 0.28 27.6
FG_SM_AF15 CCZ05738 577001.0 6453795.0 0 0.3 0.3 15.6 2.6 113 57.1 34 6.15 3.24 1.44 7.25 1.18 0.44 51.2 13.5 9.06 1.07 0.45 3.08 363.4 224.6 292.3 71.1 0.31 0.28 28.4
FG_SM_AF16 CCZ05739 577001.0 6453595.0 0 0.3 0.3 16.9 2.7 125.5 61.7 36.8 6.77 3.87 1.66 8.06 1.36 0.46 55.8 14.7 10.05 1.24 0.5 3.42 399.2 245.0 321.0 78.1 0.31 0.28 28.3
FG_SM_AF17 CCZ05740 577003.0 6453394.0 0 0.3 0.3 18.6 3.6 122.5 60 53.5 8.35 5.75 1.37 8.18 1.88 0.82 53.1 14 9.46 1.32 0.87 5.57 417.8 267.3 310.7 107.1 0.34 0.26 26.4
FG_SM_AF18 CCZ05741 577004.0 6453196.0 0 0.3 0.3 20.0 3.2 135 66.3 37.2 6.58 3.71 1.51 8.01 1.35 0.48 59 15.85 10.6 1.22 0.5 3.22 421.6 255.8 343.9 77.8 0.30 0.28 28.1
FG_SM_AF19 CCZ05742 577001.0 6452996.0 0 0.3 0.3 21.8 3.9 146.5 72.1 42.6 7.7 4.28 1.8 9.27 1.55 0.58 64 17.05 12.05 1.33 0.63 4.03 463.6 283.7 373.7 89.9 0.30 0.28 28.1
FG_SM_AF20 CCZ05743 577004.0 6452793.0 0 0.3 0.3 16.9 3.0 106 51.8 33.3 6.01 3.13 1.43 6.8 1.17 0.42 46.6 12.35 8.63 1 0.44 3.03 339.5 209.2 270.2 69.2 0.31 0.28 28.0
FG_SM_AG12 CCZ05744 577200.0 6454399.0 0 0.3 0.3 12.5 2.0 93.3 44.8 41.4 7.32 4.16 1.34 7.5 1.49 0.58 42.9 11.15 8.26 1.2 0.59 3.84 325.0 210.4 240.2 84.8 0.35 0.28 28.2
FG_SM_AG13 CCZ05745 577200.0 6454200.0 0 0.3 0.3 19.0 2.7 106 52.9 37.7 6.73 4.23 1.4 7.36 1.36 0.55 48.9 12.5 9.34 1.26 0.57 3.82 354.4 224.2 275.2 79.2 0.33 0.28 28.4
FG_SM_AG14 CCZ05746 577201.0 6454000.0 0 0.3 0.3 17.9 3.0 123.5 60.3 33.9 5.78 3.42 1.59 7.59 1.26 0.47 53 13.9 9.17 1.12 0.48 3.33 383.5 231.8 311.7 71.8 0.30 0.28 27.6
FG_SM_AG15 CCZ05747 577201.0 6453800.0 0 0.3 0.3 16.7 2.8 112 53.8 35.5 6.35 3.73 1.46 7.36 1.3 0.51 47.3 12.75 9.41 1.14 0.57 3.71 357.3 219.7 282.2 75.1 0.31 0.28 27.6
FG_SM_AG16 CCZ05748 577203.0 6453597.0 0 0.3 0.3 15.6 2.4 101 49 32.4 5.78 3.45 1.27 6.2 1.2 0.47 43.6 11.6 8.09 1.03 0.51 3.23 323.5 199.4 255.8 67.7 0.31 0.28 27.6
FG_SM_AG17 CCZ05749 577202.0 6453396.0 0 0.3 0.3 15.7 2.8 101 50.3 47.5 7.56 5.04 1.53 7.37 1.7 0.71 45 11.95 8.97 1.18 0.76 4.88 356.0 231.9 260.4 95.6 0.35 0.27 26.9
FG_SM_AG18 CCZ05750 577202.0 6453199.0 0 0.3 0.3 15.5 2.9 106 53.2 37.3 6.15 3.85 1.48 6.86 1.32 0.62 45.7 12.15 8.25 1.08 0.6 3.96 347.3 217.1 270.2 77.1 0.32 0.27 27.0
FG_SM_AG19 CCZ05751 577202.0 6452995.0 0 0.3 0.3 19.1 3.3 121 58.9 47.8 7.8 4.7 1.52 7.97 1.6 0.72 51.9 14.1 9.84 1.28 0.72 4.65 402.9 254.3 306.7 96.2 0.33 0.27 27.0
FG_SM_AG20 CCZ05752 577203.0 6452796.0 0 0.3 0.3 17.9 3.3 104.5 50.2 38.9 6.49 3.94 1.37 6.88 1.37 0.62 45.4 11.9 8.61 1.14 0.58 3.79 344.0 215.7 264.6 79.5 0.33 0.27 27.3
FG_SM_AH12 CCZ05753 577402.0 6454398.0 0 0.3 0.3 13.2 1.9 80.5 40 29.1 5.13 3.13 1.28 5.87 1.06 0.44 37 9.63 7.38 0.88 0.45 2.83 270.3 171.4 209.1 61.2 0.33 0.29 28.5
FG_SM_AH13 CCZ05754 577399.0 6454196.0 0 0.3 0.3 14.3 2.7 89.2 43.9 32.5 5.66 3.52 1.31 5.73 1.14 0.47 39.3 10.4 7.56 0.98 0.5 3.41 295.6 186.0 228.2 67.4 0.33 0.28 27.5
FG_SM_AH14 CCZ05755 577399.0 6453998.0 0 0.3 0.3 16.4 2.7 93.3 46.3 28.9 5.21 2.92 1.28 6 1.04 0.39 41.4 10.5 7.77 0.9 0.45 2.69 299.6 185.0 238.9 60.7 0.31 0.28 28.0
FG_SM_AH15 CCZ05756 577400.0 6453799.0 0 0.3 0.3 15.7 3.7 131.5 64.8 37 6.96 3.87 1.75 8.12 1.38 0.52 57.6 15.35 10.4 1.17 0.53 3.41 414.1 252.6 335.3 78.8 0.30 0.28 28.1
FG_SM_AH16 CCZ05757 577397.0 6453596.0 0 0.3 0.3 17.1 2.9 111 55.6 42.8 7.15 4.25 1.6 8.05 1.5 0.66 50.7 13.15 9.63 1.22 0.67 4.37 375.9 239.6 287.8 88.2 0.33 0.28 28.0
FG_SM_AH17 CCZ05758 577401.0 6453397.0 0 0.3 0.3 14.4 2.4 110 54.2 36.7 6.4 3.71 1.53 7.31 1.32 0.53 48.7 12.8 9.22 1.1 0.53 3.48 358.0 222.9 281.7 76.4 0.32 0.28 27.9
FG_SM_AH18 CCZ05759 577402.0 6453194.0 0 0.3 0.3 18.9 3.2 149 70.6 34.4 6.46 3.47 1.69 8.13 1.3 0.46 61.7 16.6 11.2 1.15 0.51 3.18 444.8 261.8 370.8 74.0 0.28 0.28 27.7
FG_SM_AH19 CCZ05760 577398.0 6452998.0 0 0.3 0.3 19.6 3.8 121 58.9 51.7 8.19 5.42 1.56 8.45 1.84 0.84 52.4 13.9 10.55 1.36 0.81 5.43 412.4 263.8 307.9 104.6 0.34 0.27 26.9
FG_SM_AH20 CCZ05761 577395.0 6452801.0 0 0.3 0.3 17.9 2.9 107.5 52.7 38.1 6.63 3.9 1.54 7.3 1.34 0.52 47 12.25 8.94 1.16 0.6 3.78 353.0 220.9 273.8 79.1 0.32 0.28 27.6
FG_SM_AI12 CCZ05762 577600.0 6454397.0 0 0.3 0.3 16.3 2.1 101 49 35.8 6.42 3.8 1.46 6.99 1.34 0.52 45.3 11.8 9.08 1.08 0.58 3.61 334.3 210.2 259.2 75.1 0.32 0.28 28.2
FG_SM_AI13 CCZ05763 577601.0 6454195.0 0 0.3 0.3 16.5 2.7 117.5 64.2 46.1 8.03 4.82 1.69 9.28 1.67 0.76 57.9 15.25 11 1.4 0.73 4.63 414.8 270.5 318.3 96.5 0.33 0.29 29.0
FG_SM_AI14 CCZ05764 577601.0 6453997.0 0 0.3 0.3 16.4 2.8 99.7 48.7 33.6 6.19 3.34 1.35 6.59 1.18 0.49 43.1 11.5 8.36 0.98 0.49 3.54 323.9 201.4 253.4 70.4 0.32 0.28 27.7
FG_SM_AI15 CCZ05765 577603.0 6453799.0 0 0.3 0.3 15.5 3.0 125.5 60.9 34.6 6.23 3.5 1.64 7.49 1.22 0.48 56.5 14.85 10.25 1.12 0.55 3.45 394.8 240.6 321.3 73.4 0.30 0.29 28.6
FG_SM_AI16 CCZ05766 577602.0 6453600.0 0 0.3 0.3 18.7 2.8 108.5 56.2 38.2 6.75 3.89 1.6 7.58 1.42 0.58 51.3 13.6 9.96 1.15 0.61 3.84 367.0 233.7 287.0 80.0 0.33 0.29 28.8
FG_SM_AI17 CCZ05767 577600.0 6453400.0 0 0.3 0.3 17.0 2.7 109.5 53.1 32.8 5.93 3.35 1.52 7.01 1.24 0.51 46.3 12.4 9.23 1.01 0.51 3.32 346.2 211.6 276.5 69.7 0.30 0.28 27.7
FG_SM_AI18 CCZ05768 577599.0 6453198.0 0 0.3 0.3 18.6 3.6 139 67.9 42.5 7.56 4.35 1.67 8.37 1.62 0.63 56.9 15 10.5 1.28 0.63 4.26 435.9 265.2 347.0 88.9 0.30 0.27 26.7
FG_SM_AI19 CCZ05769 577601.0 6452999.0 0 0.3 0.3 14.6 2.3 90.8 45.1 33.9 5.96 3.34 1.33 6.26 1.2 0.47 41.9 10.8 8.2 0.98 0.51 3.4 305.8 194.3 235.9 70.0 0.33 0.28 28.3
FG_SM_AI20 CCZ05770 577602.0 6452799.0 0 0.3 0.3 16.0 2.7 97.8 47.2 34.2 5.84 3.35 1.3 6.31 1.18 0.5 41.9 11.2 8.54 0.98 0.51 3.08 317.7 197.6 247.8 69.9 0.32 0.28 27.5
FG_SM_AJ12 CCZ05771 577802.0 6454397.0 0 0.3 0.3 12.6 2.0 78.9 38.9 33.8 5.67 3.39 1.29 5.94 1.19 0.53 36.9 9.32 7.25 0.94 0.5 3.31 274.3 177.4 205.3 69.1 0.35 0.28 28.1
FG_SM_AJ13 CCZ05772 577802.0 6454194.0 0 0.3 0.3 13.8 2.2 93.2 45.9 32.7 6.14 3.36 1.36 6.75 1.16 0.46 44.2 11.55 8.74 1 0.5 3.29 313.1 198.6 244.0 69.1 0.33 0.29 29.3
FG_SM_AJ14 CCZ05773 577800.0 6454000.0 0 0.3 0.3 14.8 2.9 98.6 50 35 6.17 3.66 1.3 6.43 1.29 0.48 44.3 11.7 8.41 0.99 0.56 3.49 327.8 206.6 255.3 72.4 0.32 0.28 27.8
FG_SM_AJ15 CCZ05774 577802.0 6453794.0 0 0.3 0.3 13.9 2.5 81.6 40.2 31.3 5.21 3.2 1.19 5.8 1.1 0.45 37 9.52 6.72 0.88 0.46 3.14 274.2 174.0 209.8 64.4 0.33 0.28 27.8
FG_SM_AJ16 CCZ05775 577803.0 6453599.0 0 0.3 0.3 14.5 2.5 88.9 44.6 36.4 6.13 3.65 1.32 6.35 1.25 0.57 39.9 10.15 7.7 0.95 0.57 3.85 303.8 194.6 229.2 74.5 0.34 0.27 27.4
FG_SM_AJ17 CCZ05776 577803.0 6453395.0 0 0.3 0.3 14.8 2.3 96.4 47 33 5.82 3.31 1.39 6.5 1.2 0.44 42.4 11 8.65 1.05 0.5 3.26 315.2 196.8 246.3 68.9 0.32 0.28 28.0
FG_SM_AJ18 CCZ05777 577803.0 6453196.0 0 0.3 0.3 18.7 3.1 132.5 64.1 35.3 6.35 3.33 1.52 7.66 1.26 0.46 56 15.05 10.3 1.12 0.55 3.26 407.5 244.8 333.4 74.1 0.30 0.28 27.7
FG_SM_AJ19 CCZ05778 577804.0 6452998.0 0 0.3 0.3 15.4 2.6 97.9 46.9 36.8 6.15 3.87 1.35 6.76 1.26 0.63 42.8 11.1 7.96 1.06 0.61 3.84 323.9 203.6 247.8 76.0 0.33 0.27 27.4
FG_SM_AJ20 CCZ05779 577806.0 6452797.0 0 0.3 0.3 19.0 2.7 109 52.8 35.3 6.32 3.35 1.48 7.78 1.26 0.52 48.7 12.7 9.08 1.08 0.49 3.26 352.7 218.8 278.5 74.2 0.32 0.28 28.4
FG_SM_AK12 CCZ05780 577999.0 6454401.0 0 0.3 0.3 15.1 2.5 89.1 43.1 34.2 5.45 3.5 1.28 6.25 1.21 0.51 40.5 10.8 8.19 0.93 0.5 3.46 299.7 190.3 229.8 69.9 0.33 0.28 28.1
FG_SM_AK13 CCZ05781 578003.0 6454202.0 0 0.3 0.3 12.2 2.1 76.3 37.2 29.2 5.03 2.85 1.3 5.37 1.01 0.45 34.7 9.07 7.09 0.86 0.45 2.97 257.4 163.7 197.0 60.4 0.33 0.28 28.2
FG_SM_AK14 CCZ05782 578000.0 6454000.0 0 0.3 0.3 14.0 2.6 94.4 46 42.1 6.87 4.39 1.4 6.2 1.49 0.69 41.3 10.95 7.87 1.08 0.67 4.71 325.5 209.5 240.4 85.0 0.35 0.27 26.7
FG_SM_AK15 CCZ05783 578003.0 6453798.0 0 0.3 0.3 14.9 2.4 96.6 47.6 34.8 6.12 3.56 1.52 6.82 1.25 0.57 43.5 11.6 8.91 1.04 0.51 3.39 322.2 203.6 249.6 72.7 0.33 0.28 28.3
FG_SM_AK16 CCZ05784 578001.0 6453601.0 0 0.3 0.3 14.9 2.4 99.5 48.8 37 6.11 3.69 1.48 6.92 1.27 0.54 44.1 11.9 8.58 1.06 0.55 3.53 331.1 208.9 255.2 75.9 0.33 0.28 27.8
FG_SM_AK17 CCZ05785 578003.0 6453400.0 0 0.3 0.3 14.8 2.4 90.3 44.7 35.8 5.99 3.79 1.5 6.32 1.29 0.6 40.6 10.75 7.96 0.97 0.57 3.98 307.1 196.2 232.9 74.2 0.33 0.28 27.6
FG_SM_AK18 CCZ05786 578001.0 6453200.0 0 0.3 0.3 16.7 2.8 105.5 54.8 37.9 6.53 3.83 1.45 6.98 1.32 0.59 45.5 12.2 8.79 1.06 0.56 3.87 350.1 220.5 271.9 78.2 0.32 0.27 27.1
FG_SM_AK19 CCZ05787 578003.0 6452998.0 0 0.3 0.3 16.6 2.5 102.5 49.2 34.9 6.03 3.59 1.42 7.02 1.27 0.46 46 12.3 8.74 1.02 0.48 3.33 334.9 209.0 262.3 72.6 0.32 0.28 28.3
FG_SM_AK20 CCZ05788 578003.0 6452793.0 0 0.3 0.3 19.2 3.0 127.5 61.5 36.4 6.41 3.46 1.84 8.02 1.28 0.48 58.3 15.7 10.95 1.2 0.48 3.32 405.1 248.5 328.4 76.7 0.31 0.29 29.1
FG_SM_AL12 CCZ05789 578197.0 6454400.0 0 0.3 0.3 14.4 2.0 84.5 42 31.5 5.59 3.19 1.43 6.39 1.17 0.45 38.5 10.2 7.81 0.96 0.47 3.08 285.5 181.7 219.3 66.1 0.33 0.28 28.4
FG_SM_AL13 CCZ05790 578199.0 6454196.0 0 0.3 0.3 11.6 1.9 74.2 38 31.9 4.89 3.09 1.28 5.46 1.06 0.48 34.2 8.88 6.49 0.85 0.44 3.02 258.0 166.8 193.9 64.1 0.34 0.28 27.5
FG_SM_AL14 CCZ05791 578199.0 6453998.0 0 0.3 0.3 12.6 2.1 86.3 42.5 33.8 5.73 3.48 1.34 6.02 1.22 0.49 39.9 10.65 7.84 0.99 0.49 3.53 294.0 188.0 224.4 69.7 0.34 0.28 28.3
FG_SM_AL15 CCZ05792 578199.0 6453798.0 0 0.3 0.3 15.0 2.3 121.5 63.4 33.6 5.58 3.26 1.5 6.53 1.14 0.47 51.9 14.9 8.81 0.98 0.48 3.21 381.6 232.4 312.4 69.3 0.29 0.27 27.2
FG_SM_AL16 CCZ05793 578200.0 6453600.0 0 0.3 0.3 13.2 2.7 107 55.9 33.4 5.83 3.31 1.46 7 1.19 0.47 47.4 13.1 8.9 1.03 0.48 3.22 348.4 217.0 278.4 70.0 0.31 0.28 28.0
FG_SM_AL17 CCZ05794 578200.0 6453400.0 0 0.3 0.3 20.1 3.3 137.5 66.9 39.3 7.07 4.07 1.83 8.71 1.44 0.55 62 16.95 11.85 1.22 0.56 3.56 437.1 268.2 353.9 83.2 0.31 0.29 28.9
FG_SM_AL18 CCZ05795 578198.0 6453200.0 0 0.3 0.3 21.6 3.5 130.5 62.6 44 7.35 4.67 1.63 8.11 1.51 0.72 57.9 15.4 10.75 1.22 0.69 4.59 423.2 262.9 332.3 90.9 0.32 0.28 27.8
FG_SM_AL19 CCZ05796 578202.0 6452996.0 0 0.3 0.3 16.5 2.5 97.6 50.1 42.7 6.97 4.4 1.62 7.35 1.48 0.64 46.6 11.95 9.15 1.2 0.63 4.2 345.0 225.1 258.1 86.9 0.35 0.28 28.2
FG_SM_AL20 CCZ05797 578206.0 6452796.0 0 0.3 0.3 18.4 3.4 125.5 59.4 33.7 5.89 3.37 1.42 6.8 1.18 0.52 51.5 14.1 9.62 1.03 0.52 3.39 382.6 228.4 312.1 70.5 0.29 0.27 27.2
FG_SM_AM12 CCZ05798 578401.0 6454397.0 0 0.3 0.3 14.3 2.3 91.7 45.1 35 5.9 3.43 1.44 6.43 1.18 0.52 41.8 11.05 8 0.97 0.52 3.44 308.7 196.1 236.9 71.8 0.33 0.28 28.1
FG_SM_AM13 CCZ05799 578398.0 6454195.0 0 0.3 0.3 13.4 1.9 74.9 37 28.8 4.96 2.98 1.35 5.42 1.01 0.42 34.4 9.21 7.06 0.86 0.43 3 254.9 162.9 194.8 60.0 0.33 0.28 28.4
FG_SM_AM14 CCZ05800 578402.0 6453997.0 0 0.3 0.3 16.9 2.1 90.1 42.7 33.7 5.48 3.28 1.24 5.89 1.14 0.45 40.9 10.65 8.18 0.92 0.42 3.12 298.8 188.1 230.8 68.0 0.33 0.28 28.2
FG_SM_AM15 CCZ05801 578400.0 6453800.0 0 0.3 0.3 13.7 2.3 117 57 41.3 6.92 4 1.44 7.23 1.43 0.55 47.7 12.9 9.4 1.15 0.58 3.99 376.5 232.8 292.7 83.8 0.32 0.26 26.5
FG_SM_AM16 CCZ05802 578401.0 6453596.0 0 0.3 0.3 22.6 3.6 115 56.6 31.1 5.8 3.28 1.22 6.9 1.15 0.46 48.4 13.55 9.59 1.06 0.46 3.14 358.0 216.8 291.6 66.5 0.29 0.28 27.9
FG_SM_AM17 CCZ05803 578402.0 6453395.0 0 0.3 0.3 12.3 2.6 82.5 40.1 29.7 5.05 2.97 1.19 5.54 1.1 0.47 36.3 9.76 7.47 0.84 0.46 2.98 272.5 171.2 211.2 61.4 0.32 0.28 27.9
FG_SM_AM18 CCZ05804 578398.0 6453196.0 0 0.3 0.3 16.4 3.5 106 53.1 41.4 7.04 4.2 1.7 7.76 1.47 0.62 49.9 12.95 9.76 1.2 0.61 3.82 362.9 232.7 277.7 85.2 0.34 0.29 28.6
FG_SM_AM19 CCZ05805 578400.0 6452994.0 0 0.3 0.3 14.9 3.1 96.6 48.1 34.7 5.77 3.49 1.35 6.24 1.21 0.5 43.3 11.25 8.36 1.02 0.53 3.3 319.8 201.2 248.9 71.0 0.33 0.28 27.8
FG_SM_AM20 CCZ05806 578402.0 6452797.0 0 0.3 0.3 16.6 2.6 99.9 53 37.1 6 3.63 1.5 7.02 1.29 0.51 45 12.15 8.79 1.08 0.49 3.37 337.9 215.2 262.2 75.7 0.32 0.28 27.7
FG_SM_AN12 CCZ05807 578598.0 6454396.0 0 0.3 0.3 13.9 2.2 76.5 37.8 36.7 5.74 3.64 1.16 6.03 1.27 0.59 35.5 9.45 7.17 0.95 0.56 3.72 273.2 179.2 199.4 73.8 0.36 0.28 27.7
FG_SM_AN13 CCZ05808 578600.0 6454197.0 0 0.3 0.3 15.2 2.3 84.9 43 37.1 6.28 3.82 1.22 6.42 1.35 0.57 40.3 10.6 7.92 0.99 0.57 3.97 299.8 195.5 223.7 76.0 0.35 0.28 28.3
FG_SM_AN14 CCZ05809 578600.0 6453994.0 0 0.3 0.3 16.9 3.0 113 58.1 51 8.69 5.24 1.28 8.76 1.82 0.75 53.6 14.2 10.2 1.36 0.78 5.27 402.2 263.4 298.5 103.7 0.35 0.28 28.1
FG_SM_AN15 CCZ05810 578599.0 6453795.0 0 0.3 0.3 19.5 5.5 113.5 55.4 43.2 7.4 4.41 1.47 7.3 1.47 0.73 49 12.95 9.25 1.19 0.71 4.8 376.6 237.2 287.9 88.7 0.33 0.27 27.0
FG_SM_AN16 CCZ05811 578599.0 6453597.0 0 0.3 0.3 13.3 2.8 100.5 49.8 31.7 5.53 3.12 1.32 6.13 1.08 0.52 44 11.85 8.22 0.95 0.45 3.34 323.1 199.6 257.0 66.0 0.31 0.28 27.8
FG_SM_AN17 CCZ05812 578600.0 6453397.0 0 0.3 0.3 13.5 2.6 94 44.6 37.6 6.16 3.54 1.58 7.17 1.35 0.54 42.3 10.85 8.36 1.06 0.59 3.81 317.3 201.8 239.9 77.4 0.34 0.28 28.0
FG_SM_AN18 CCZ05813 578603.0 6453197.0 0 0.3 0.3 14.2 2.4 87 42.6 34.8 5.73 3.57 1.2 6.32 1.22 0.54 39.2 10.35 7.64 0.99 0.54 3.42 295.1 188.3 223.9 71.2 0.34 0.28 27.8
FG_SM_AN19 CCZ05814 578599.0 6452996.0 0 0.3 0.3 15.2 3.3 104 51.5 38.7 6.83 4.15 1.64 7.36 1.44 0.55 46.9 12.55 9.19 1.18 0.58 3.59 349.2 221.4 268.7 80.5 0.33 0.28 28.1
FG_SM_AN20 CCZ05815 578600.0 6452794.0 0 0.3 0.3 16.9 3.0 99.3 50.4 38.9 6.37 4.14 1.46 7.01 1.42 0.57 46 12.35 8.75 1.14 0.62 3.75 339.6 217.6 259.8 79.8 0.33 0.28 28.1
FG_SM_V22 CCZ05816 574999.0 6452396.0 0 0.3 0.3 15.9 2.3 95.6 46.8 32.9 5.6 3.69 1.25 6.19 1.17 0.47 45.5 11.35 8.64 0.93 0.55 2.95 317.1 199.7 249.1 68.0 0.33 0.29 28.8
FG_SM_V24 CCZ05817 575004.0 6451998.0 0 0.3 0.3 19.3 2.8 104 50.8 30.7 5.76 3.46 1.34 6.99 1.15 0.44 47.8 12 9.51 1.04 0.42 2.64 334.3 206.5 268.6 65.7 0.31 0.29 29.1
FG_SM_V26 CCZ05818 575000.0 6451593.0 0 0.3 0.3 12.9 1.9 65.3 33.9 23.7 4.3 2.71 0.91 4.61 0.89 0.37 32.1 7.83 6.3 0.71 0.37 2.31 224.0 143.8 174.2 49.8 0.33 0.29 29.1
FG_SM_V28 CCZ05819 574997.0 6451196.0 0 0.3 0.3 14.2 2.2 77.7 39.1 32.1 5.26 3.59 1.14 5.92 1.16 0.53 38.6 9.68 7.32 0.89 0.55 3.13 272.7 177.3 206.5 66.2 0.35 0.29 29.0
FG_SM_V30 CCZ05820 575000.0 6450798.0 0 0.3 0.3 12.8 1.9 71.5 35.7 27.9 4.76 3.18 1.12 5.29 1.02 0.44 35 8.7 6.8 0.79 0.44 2.79 247.1 159.3 188.9 58.2 0.34 0.29 29.0
FG_SM_X22 CCZ05821 575400.0 6452404.0 0 0.3 0.3 14.9 2.4 99.5 46.8 28.5 5.07 3.07 1.56 6.69 1.03 0.38 46.6 11.7 9.41 0.93 0.4 2.41 317.5 195.2 256.5 60.9 0.31 0.30 29.6
FG_SM_X24 CCZ05822 575401.0 6452002.0 0 0.3 0.3 16.4 1.9 65.9 33.5 26 4.08 2.73 1.01 5.02 0.94 0.39 32.6 8 6.02 0.76 0.36 2.36 228.2 147.3 174.9 53.3 0.34 0.29 28.9
FG_SM_X26 CCZ05823 575398.0 6451601.0 0 0.3 0.3 15.6 2.6 112 50.7 35.2 6.31 4.16 1.68 7.48 1.37 0.53 51.2 13.2 9.88 1.11 0.59 3.22 359.3 221.7 284.2 75.1 0.32 0.29 29.0
FG_SM_X28 CCZ05824 575404.0 6451203.0 0 0.3 0.3 17.5 2.9 97.4 46.5 33.8 5.53 3.97 1.16 6.63 1.26 0.54 44 11.5 8.69 0.99 0.51 3.46 320.0 200.4 249.5 70.5 0.32 0.28 28.3
FG_SM_X30 CCZ05825 575398.0 6450803.0 0 0.3 0.3 15.4 2.4 77.4 37.5 31.4 5.02 3.39 1.04 5.51 1.06 0.45 36 9.23 6.81 0.87 0.48 2.88 263.7 168.7 200.1 63.6 0.34 0.28 28.1
FG_SM_Z22 CCZ05826 575800.0 6452401.0 0 0.3 0.3 17.0 2.8 101 48.3 30.1 5.37 3.15 1.25 6.53 1.14 0.43 45.6 11.75 9.2 0.97 0.43 2.76 322.3 198.2 258.8 63.5 0.31 0.29 28.8
FG_SM_Z24 CCZ05827 575803.0 6451997.0 0 0.3 0.3 14.6 2.3 100 48.8 29.9 5.33 3.53 1.5 6.65 1.12 0.42 47.2 12.35 9.19 0.94 0.44 2.64 324.6 201.8 260.7 63.9 0.31 0.29 29.4
FG_SM_Z26 CCZ05828 575798.0 6451599.0 0 0.3 0.3 17.2 2.8 100.5 47.7 36.9 6.12 4.45 1.28 6.65 1.38 0.59 46.4 11.75 8.64 1.03 0.57 3.63 334.1 210.6 257.7 76.4 0.33 0.28 28.2
FG_SM_Z28 CCZ05829 575801.0 6451202.0 0 0.3 0.3 15.7 2.4 91.7 45.4 34 5.77 3.97 1.2 6.48 1.2 0.5 45 11.25 8.5 0.97 0.51 3.35 312.5 199.9 241.8 70.7 0.34 0.29 29.2
FG_SM_Z30 CCZ05830 575802.0 6450799.0 0 0.3 0.3 15.3 2.4 80.9 41.4 33.2 5.66 3.83 1.3 6.33 1.24 0.49 40.3 10 7.73 0.98 0.51 3.41 285.4 186.0 216.0 69.4 0.34 0.29 29.1
FG_SM_AB22 CCZ05831 576199.0 6452399.0 0 0.3 0.3 13.0 2.4 82.9 41.2 28 5 3.17 1.41 5.57 0.97 0.33 38.6 9.6 7.18 0.8 0.41 2.45 273.8 171.9 215.1 58.7 0.32 0.29 28.5
FG_SM_AB24 CCZ05832 576198.0 6451999.0 0 0.3 0.3 18.0 3.1 108 50.8 34.6 6.03 3.64 1.4 6.95 1.2 0.51 48 12.2 9.16 1.07 0.49 3.33 345.8 213.1 273.6 72.2 0.32 0.28 28.2
FG_SM_AB26 CCZ05833 576201.0 6451598.0 0 0.3 0.3 16.8 2.5 96.5 49.3 33.3 5.83 3.78 1.32 6.93 1.2 0.51 48.7 12.1 8.73 1 0.53 2.99 327.9 209.3 257.9 70.0 0.33 0.30 29.7
FG_SM_AB28 CCZ05834 576201.0 6451197.0 0 0.3 0.3 15.6 2.6 106.5 50.7 32.6 5.7 3.71 1.51 6.67 1.18 0.43 49.6 12.35 9.57 1.03 0.49 2.94 342.7 211.9 274.2 68.6 0.32 0.29 29.0
FG_SM_AB30 CCZ05835 576201.0 6450798.0 0 0.3 0.3 12.4 1.9 66.5 32 29.4 4.62 3.41 1.12 5.22 1.02 0.39 33.1 7.8 6.39 0.86 0.46 2.71 234.7 153.1 174.7 60.1 0.36 0.29 28.9
FG_SM_POC CCZ05836 575129.0 6451468.0 0 0.3 0.3 18.0 2.9 103.5 52.2 36.1 5.57 4.15 1.5 7.31 1.28 0.6 49.9 12.8 9.52 1.06 0.61 3.64 348.4 221.3 273.1 75.4 0.33 0.29 28.9
Notes:
1. Verification has been undertaken by CCZ
Geology team personnel.
2. Sample results from ALS method ME-ICP81.
Source: ALS Adelaide.
APPENDIX D: JORC CODE, 2012 EDITION - TABLE 1 - FENCE GOSSAN SURFACE SAMPLING
Section 1: Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling techniques Nature and quality of sampling (e.g., cut channels, random chips, or specific Diamond Drilling (DDH)
specialised industry standard measurement tools appropriate to the minerals
under investigation, such as down hole gamma sondes, or handheld XRF Diamond drilling of HQ diameter (TT_005DD) was completed to 137.7m recently in
instruments, etc.). These examples should not be taken as limiting the broad the completed program and was located 5m away from a RC hole already drilled
meaning of sampling. (TT_003RC).
Include reference to measures taken to ensure sample representivity and the Reverse Circulation ('RC') Drilling
appropriate calibration of any measurement tools or systems used.
RC drilling at Fence Gossan was used to obtain a representative sample by
Aspects of the determination of mineralisation that are Material to the Public means of riffle splitting with samples submitted for analysis using the
Report. above-mentioned methodologies.
In cases where 'industry standard' work has been done this would be relatively Four (4) reverse circulation (RC) holes for a total of 516m have been
simple (e.g., 'reverse circulation drilling was used to obtain 1 m samples completed at the Fence Gossan Prospect.
from which 3 kg was pulverised to produce a 30g charge for fire assay'). In
other cases, more explanation may be required, such as where there is coarse Four (4) RC holes were completed at Reefs Tank for a total of 564m.
gold that has inherent sampling problems. Unusual commodities or
mineralisation types (eg submarine nodules) may warrant disclosure of detailed At Tors Tank, four (4) RC holes for a total of 625.7m (including the cored
information. hole) were completed.
The RC drilling technique was used to obtain a representative sample by means
of a cone or riffle splitter with samples submitted for assay by mixed acid
digestion and analysis via ICP-MS + ICP-AES with anticipated reporting a suite
of 48 elements (sulphur >10% by LECO)
Surface Sampling
Two large surface sampling programs were conducted on grids based about the
drilling at Tors Tank and Fence Gossan. The sampling was by using hand auger
to take soil samples from depth varying between 0.1-0.5m. Original samples
were between 0.5-2kg in weight, reduced to 200g for crushing and
pulverizing. The Stage 1 program consisted of 189 sampling stations, spaced
at 200m intervals across a total survey area measuring 6.4km(2)
The first area was based about the centre of the grid, closest to the known
points of observations (drill holes FG001RC-4RC). Stations extended east of
the Resource Mask to the EL8434 lease boundary. Stations also extended west
to identify extension of REEs into the Reef Tank Resource Area. Station
numbers are based on a wider grid that incorporates Reef Tank and Tors Tank.
A Stage 2 second area at a larger spacing (400m) was completed slighter later
in December 2022, which managed to collect another 21 samples over mainly
pegmatite outcrop.
Drilling techniques Drill type (e.g., core, reverse circulation, open-hole hammer, rotary air Historical drilling consisted of auger, rotary air blast, reverse circulation,
blast, auger, Bangka, sonic, etc.) and details (e.g., core diameter, triple or and NQ, BQ, and HQ diamond coring. One cored hole of HQ (61mm) diameter was
standard tube, depth of diamond tails, face-sampling bit or other type, completed at Tors Tank after all the RC holes had been completed.
whether core is oriented and if so, by what method, etc.).
Diamond drilling was completed with standard diameter, conventional HQ, with
historical holes typically utilizing RC and percussion pre-collars to an
average 30 metres (see drillhole information for further details).
Drill sample recovery Method of recording and assessing core and chip sample recoveries and results Reverse Circulation ('RC') Drilling - Reverse circulation sample recoveries
assessed. were visually estimated during drilling programs. Where the estimated sample
recovery was below 100% this was recorded in field logs by means of
Measures taken to maximise sample recovery and ensure representative nature of qualitative observation.
the samples.
Reverse circulation drilling employed sufficient air (using a compressor and
Whether a relationship exists between sample recovery and grade and whether booster) to maximise sample recovery. Historical cored drillholes by North
sample bias may have occurred due to preferential loss/gain of fine/coarse Broken Hill, CRA , and Pasminco were well documented and generally have
material. >90% core recovery.
No relationship between sample recovery and grade has been observed.
Logging Whether core and chip samples have been geologically and geotechnically logged The drilling that did occur was completed to modern-day standards. The
to a level of detail to support appropriate Mineral Resource estimation, preferred exploration strategy in the eighties and early nineties was to drill
mining studies and metallurgical studies. shallow auger holes to negate the influence of any Quaternary and Tertiary
sedimentary cover, and then return to sites where anomalous Cu or Zn were
Whether logging is qualitative or quantitative in nature. Core (or costean, assayed. In this program at all three areas holes were completed to varying
channel, etc) photography. depths ranging from 100-160m.
The total length and percentage of the relevant intersections logged. No downhole geophysical logging took place; however, measurements of magnetic
susceptibility were taken at the same 1m intervals as the PXRF readings were
taken.
Sub-sampling techniques and sample preparation If core, whether cut or sawn and whether quarter, half or all core taken. Core samples will be hand-split or sawn with re-logging of available
historical core indicating a 70:30 (retained: assayed) split was typical. The
If non-core, whether riffled, tube sampled, rotary split, etc and whether variation of sample ratios noted are considered consistent with the
sampled wet or dry. sub-sampling technique (hand-splitting).
For all sample types, the nature, quality, and appropriateness of the sample No second half samples will be submitted for analysis, but duplicates have
preparation technique. been taken at a frequency of 1:20 in samples collected.
Quality control procedures adopted for all sub-sampling stages to maximise It is considered water planned to be used for core cutting is unprocessed and
representivity of samples. unlikely to have introduced sample contamination.
Measures taken to ensure that the sampling is representative of the in-situ Procedures relating to the definition of the line of cutting or splitting are
material collected, including for instance results for field not available. It is expected that 'standard industry practice' for the
duplicate/second-half sampling. period was applied to maximize sample representivity.
Whether sample sizes are appropriate to the grain size of the material being Quarter core will be submitted to ALS for chemical analysis using industry
sampled. standard sample preparation and analytical techniques.
The sample interval details and grades quoted for cored intervals described in
various maps in the main section are given in previous ASX releases (Castillo
Copper 2022a, b, c, d, e, f, g).
Quality of assay data and laboratory tests The nature, quality and appropriateness of the assaying and laboratory The following rare earth elements were analysed using ME-MS61R Sample
procedures used and whether the technique is considered partial or total. Decomposition is by HF-HNO(3)-HClO(4) acid digestion, HCl leach (GEO-4A01).
The Analytical Method for
For geophysical tools, spectrometers, handheld XRF instruments, etc, the
parameters used in determining the analysis including instrument make and Silver is shown below:
model, reading times, calibrations factors applied and their derivation, etc.
Element Symbol Units Lower Limit Upper Limit
Silver Ag ppm 0.01 100
Nature of quality control procedures adopted (eg standards, blanks,
duplicates, external laboratory checks) and whether acceptable levels of
Inductively Coupled Plasma - Atomic Emission Spectroscopy (ICP - AES)
accuracy (i.e. lack of bias) and precision have been established. Inductively Coupled Plasma - Mass Spectrometry (ICP-MS)
Aprepared sample (0.25 g) is digested with perchloric, nitric, hydrofluoric,
and hydrochloric acids. The residue is topped up with dilute hydrochloric acid
and analysed by inductively coupled plasma atomic emission spectrometry.
Following this analysis, the results are reviewed for high concentrations of
bismuth, mercury, molybdenum, silver, and tungsten and diluted accordingly.
Samples meeting this criterion are then analysed by inductively coupled
plasma-mass spectrometry. Results are corrected for spectral interelement
interferences.
Four acid digestions can dissolve most minerals: however, although the term
"near total" is used, depending on the sample matrix, not all elements are
quantitatively extracted.
Results for the additional rare earth elements will represent the acid
leachable portion of the rare earth elements and as such, cannot be used, for
instance to do a chondrite plot.
Geochemical Procedure
Element geochemical procedure reporting units and limits are listed below:
Element Symbol Units Lower Limit Upper Limit
Aluminum Al % 0.01 50
Arsenic As ppm 0.2 10 000
Barium Ba ppm 10 10 000
Beryllium Be ppm 0.05 1 000
Bismuth Bi ppm 0.01 10 000
Calcium Ca % 0.01 50
Cadmium Cd ppm 0.02 1 000
Cerium Ce ppm 0.01 500
Cobalt Co ppm 0.1 10 000
Chromium Cr ppm 1 10 000
Cesium Cs ppm 0.05 500
Copper Cu ppm 0.2 10 000
Iron Fe % 0.01 50
Gallium Ga ppm 0.05 10 000
Germanium Ge ppm 0.05 500
Hafnium Hf ppm 0.1 500
Indium In ppm 0.005 500
Potassium K % 0.01 10
Lanthanum La ppm 0.5 10 000
Lithium Li ppm 0.2 10 000
Magnesium Mg % 0.01 50
Manganese Mn ppm 5 100 000
Element Symbol Units Lower Limit Upper Limit
Molybdenum Mo ppm 0.05 10 000
Sodium Na % 0.01 10
Niobium Nb ppm 0.1 500
Nickel Ni ppm 0.2 10 000
Phosphorous P ppm 10 10 000
Lead Pb ppm 0.5 10 000
Rubidium Rb ppm 0.1 10 000
Rhenium Re ppm 0.002 50
Sulphur S % 0.01 10
Antimony Sb ppm 0.05 10 000
Scandium Sc ppm 0.1 10 000
Selenium Se ppm 1 1 000
Tin Sn ppm 0.2 500
Strontium Sr ppm 0.2 10 000
Tantalum Ta ppm 0.05 100
Tellurium Te ppm 0.05 500
Thorium Th ppm 0.2 10 000
Titanium Ti % 0.005 10
Thallium Tl ppm 0.02 10 000
Uranium U ppm 0.1 10 000
Vanadium V ppm 1 10 000
Tungsten W ppm 0.1 10 000
Method ME-MS81
This method involves a lithium borate fusion prior to acid dissolution and
ICP- MS analysis provides the most quantitative analytical approach for a
broad suite of trace elements. Options for adding the whole rock elements
from an |CP - AES analysis on the same fusion, or base metals from a separate
four acid digestion, are available.
Lower and upper detection limits are given below:
Element Symbol Units Lower Limit Upper Limit
Yttrium Y ppm 0.1 500
Zinc Zn ppm 2 10 000
Zirconium Zr ppm 0.5 500
Dysprosium Dy ppm 0.05 1 000
Erbium Er ppm 0.03 1 000
Europium Eu ppm 0.03 1 000
Gadolinium Gd ppm 0.05 1 000
Holmium Ho ppm 0.01 1 000
Lutetium Lu ppm 0.01 1 000
Neodymium Nd ppm 0.1 1 000
Praseodymium Pr ppm 0.03 1 000
Samarium Sm ppm 0.03 1 000
Terbium Tb ppm 0.01 1 000
Thulium Tm ppm 0.01 1 000
Ytterbium Yb ppm 0.03 1 000
Inductively Coupled Plasma - Atomic Emission Spectroscopy (ICP - AES)
Inductively Coupled Plasma - Mass Spectrometry (ICP-MS)
A prepared sample (0.25 g) is digested with perchloric, nitric, hydrofluoric,
and hydrochloric acids. The residue is topped up with dilute hydrochloric acid
and analysed by inductively coupled plasma atomic emission spectrometry.
Following this analysis, the results are reviewed for high concentrations of
bismuth, mercury, molybdenum, silver, and tungsten and diluted accordingly.
Samples meeting this criterion are then analysed by inductively coupled
plasma-mass spectrometry. Results are corrected for spectral interelement
interferences.
Four acid digestions can dissolve most minerals: however, although the term
"near total" is used, depending on the sample matrix, not all elements are
quantitatively extracted.
Results for the additional rare earth elements will represent the acid
leachable portion of the rare earth elements and as such, cannot be used, for
instance to do a chondrite plot.
Geochemical Procedure
Element geochemical procedure reporting units and limits are listed below:
Element Symbol Units Lower Limit Upper Limit
Aluminum Al % 0.01 50
Arsenic As ppm 0.2 10 000
Barium Ba ppm 10 10 000
Beryllium Be ppm 0.05 1 000
Bismuth Bi ppm 0.01 10 000
Calcium Ca % 0.01 50
Cadmium Cd ppm 0.02 1 000
Cerium Ce ppm 0.01 500
Cobalt Co ppm 0.1 10 000
Chromium Cr ppm 1 10 000
Cesium Cs ppm 0.05 500
Copper Cu ppm 0.2 10 000
Iron Fe % 0.01 50
Gallium Ga ppm 0.05 10 000
Germanium Ge ppm 0.05 500
Hafnium Hf ppm 0.1 500
Indium In ppm 0.005 500
Potassium K % 0.01 10
Lanthanum La ppm 0.5 10 000
Lithium Li ppm 0.2 10 000
Magnesium Mg % 0.01 50
Manganese Mn ppm 5 100 000
Element Symbol Units Lower Limit Upper Limit
Molybdenum Mo ppm 0.05 10 000
Sodium Na % 0.01 10
Niobium Nb ppm 0.1 500
Nickel Ni ppm 0.2 10 000
Phosphorous P ppm 10 10 000
Lead Pb ppm 0.5 10 000
Rubidium Rb ppm 0.1 10 000
Rhenium Re ppm 0.002 50
Sulphur S % 0.01 10
Antimony Sb ppm 0.05 10 000
Scandium Sc ppm 0.1 10 000
Selenium Se ppm 1 1 000
Tin Sn ppm 0.2 500
Strontium Sr ppm 0.2 10 000
Tantalum Ta ppm 0.05 100
Tellurium Te ppm 0.05 500
Thorium Th ppm 0.2 10 000
Titanium Ti % 0.005 10
Thallium Tl ppm 0.02 10 000
Uranium U ppm 0.1 10 000
Vanadium V ppm 1 10 000
Tungsten W ppm 0.1 10 000
Method ME-MS81
This method involves a lithium borate fusion prior to acid dissolution and
ICP- MS analysis provides the most quantitative analytical approach for a
broad suite of trace elements. Options for adding the whole rock elements
from an |CP - AES analysis on the same fusion, or base metals from a separate
four acid digestion, are available.
Lower and upper detection limits are given below:
Element Symbol Units Lower Limit Upper Limit
Yttrium Y ppm 0.1 500
Zinc Zn ppm 2 10 000
Zirconium Zr ppm 0.5 500
Dysprosium Dy ppm 0.05 1 000
Erbium Er ppm 0.03 1 000
Europium Eu ppm 0.03 1 000
Gadolinium Gd ppm 0.05 1 000
Holmium Ho ppm 0.01 1 000
Lutetium Lu ppm 0.01 1 000
Neodymium Nd ppm 0.1 1 000
Praseodymium Pr ppm 0.03 1 000
Samarium Sm ppm 0.03 1 000
Terbium Tb ppm 0.01 1 000
Thulium Tm ppm 0.01 1 000
Ytterbium Yb ppm 0.03 1 000
· Laboratory inserted standards, blanks and duplicates were
analysed per industry standard practice. There was no evidence of bias from
these results.
Verification of sampling and assaying The verification of significant intersections by either independent or · Two of the drillholes have been twinned, at Tors Tank where
alternative company personnel. TT_005DD was drilled next to TT_003RC.
The use of twinned holes. · Conversion of elemental analysis (REE parts per million) to
stoichiometric oxide (REO parts per million) was undertaken by ROM geological
Documentation of primary data, data entry procedures, data verification, data staff using the below element to stoichiometric oxide conversion factors
storage (physical and electronic) protocols. (https://www.jcu.edu.au/news/releases/2020/march/rare-earth-metals-an-untapped-resource
(https://www.jcu.edu.au/news/releases/2020/march/rare-earth-metals-an-untapped-resource)
Discuss any adjustment to assay data. )
Table C1-1: Element -Conversion Factor -Oxide Form
Ce 1.2284 CeO(2)
Dy 1.1477 Dy(2)O(3)
Er 1.1435 Er(2)O(3)
Eu 1.1579 Eu(2)O(3)
Gd 1.1526 Gd(2)O(3)
Ho 1.1455 Ho(2)O(3)
La 1.1728 La(2)O(3)
Lu 1.1371 Lu(2)O(3)
Nd 1.1664 Nd(2)O(3)
Pr 1.2083 Pr(6)O(11)
Sm 1.1596 Sm(2)O(3)
Tb 1.1762 Tb(4)O(7)
Tm 1.1421 Tm(2)O(3)
Y 1.2699 Y(2)O(3)
Yb 1.1387 Yb(2)O(3)
Rare earth oxide is the industry accepted form for reporting rare earths. The
following calculations are used for compiling REO into their reporting and
evaluation groups:
TREO (Total Rare Earth Oxide) = La(2)O(3) + CeO(2) + Pr(6)O(11) + Nd(2)O(3) +
Sm(2)O(3) + Eu(2)O(3) + Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3) + Ho(2)O(3) +
Er(2)O(3) + Tm(2)O(3) + Yb(2)O(3) + Y(2)O(3) + Lu(2)O(3).
TREO-Ce = TREO - CeO(2)
LREO (Light Rare Earth Oxide) = La(2)O(3) + CeO(2) + Pr(6)O(11) + Nd(2)O(3) +
Sm(2)O(3)
HREO (Heavy Rare Earth Oxide) = Eu(2)O(3) + Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3)
+ Ho(2)O(3) + Er(2)O(3) + Tm2O3 + Yb2O3 + Y2O3 + Lu2O3
CREO (Critical Rare Earth Oxide) = Nd(2)O(3) + Eu(2)O(3) + Tb(4)O(7) +
Dy(2)O(3) + Y(2)O(3)
MREO (Magnetic Rare Earth Oxide) = Pr(6)O(11) + Nd(2)O(3) + Sm(2)O(3) +
Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3).
Total Rare Earth Oxides (TREO):
To calculate TREO an oxide conversion "factor" is applied to each rare-earth
element assay. The "factor" equates an elemental assay to an oxide
concentration for each element. Below is an example of the factor calculation
for Lanthanum (La):
o Relative Atomic Mass (La) = 138.9055
o Relative Atomic Mass (O) = 15.9994
o Oxide Formula = La(2)O(3)
o Oxide Conversion Factor = 1/ ((2x 138.9055)/(2x 138.9055 + 3x 15.9994))
Oxide Conversion Factor = 1.173 (3dp)
None of the historical data has been adjusted.
Location of data points Accuracy and quality of surveys used to locate drill holes (collar and In general, locational accuracy does vary, depending upon whether the
down-hole surveys), trenches, mine workings and other locations used in historical surface and drillhole samples were digitised off plans or had their
Mineral Resource estimation. coordinated tabulated. Many samples were originally reported to AGD66 or
AMG84 and have been converted to MGA94 (Zone 54)
Specification of the grid system used.
The holes are currently surveyed with handheld GPS, awaiting more accurate
Quality and adequacy of topographic control. DGPS survey. It is thus estimated that locational accuracy therefore varies
between 2-4m until the more accurate surveying is completed. This assessment
was confirmed once the holes were surveyed by DGPS from GMC Surveying.
The quality of topographic control (GSNSW 1 sec DEM) is deemed adequate for
the purposes of the exploration drilling program.
Data spacing and distribution Data spacing for reporting of Exploration Results. The average sample spacing from the current drilling program across the tenure
varies per prospect, and sample type, as listed in Table C1-2, below:
Whether the data spacing and distribution is sufficient to establish the
degree of geological and grade continuity appropriate for the Mineral Resource Table C1-2: EL 8434 Drillhole Spacing
and Ore Reserve estimation procedure(s) and classifications applied.
Prospect Drillholes Completed RMS Drillhole Spacing (m)
The Sisters Not yet
Whether sample compositing has been applied. Iron Blow Not Yet
Tors Tank 4 127
Fence Gossan 4 208
Ziggy's Hill n/a n/a
Reefs Tank 4 221
The Datamine software allows creation of fixed length samples from the
original database given a set of stringent rules.
Sample location is shown in Figure C1.
Figure C1: Location of Stage 1 Fence Gossan Surface Samples
Orientation of data in relation to geological structure Whether the orientation of sampling achieves unbiased sampling of possible Historical drill holes at the BHAE are typically drilled vertically for auger
structures and the extent to which this is known, considering the deposit and RAB types (drilled along section lines) and angled at -55˚ or -60˚ to
type. the horizontal and drilled perpendicular to the mineralised trend for RC and
DDH.
If the relationship between the drilling orientation and the orientation of
key mineralised structures is considered to have introduced a sampling bias, Drilling orientations are adjusted along strike to accommodate folded
this should be assessed and reported if material. geological sequences. All Fence Gossan holes were designed to drill toward
grid south at an inclination of 60 degrees from horizontal.
The drilling orientation is not considered to have introduced a sampling bias
on assessment of the current geological interpretation.
Geological mapping by various companies has reinforced that the strata dips
variously between 5 and 65 degrees.
Sample security The measures taken to ensure sample security. Sample security procedures are considered 'industry standard' for the current
period.
Samples obtained during drilling completed between 4/10/22 to the 10/10/22
were transported by exploration employees or an independent courier directly
from Broken Hill to ALS Laboratory, Adelaide.
The Company considers that risks associated with sample security are limited
given the nature of the targeted mineralisation.
Audits or reviews The results of any audits or reviews of sampling techniques and data. No external audits or reviews have yet been undertaken.
Inductively Coupled Plasma - Atomic Emission Spectroscopy (ICP - AES)
Inductively Coupled Plasma - Mass Spectrometry (ICP-MS)
A prepared sample (0.25 g) is digested with perchloric, nitric, hydrofluoric,
and hydrochloric acids. The residue is topped up with dilute hydrochloric acid
and analysed by inductively coupled plasma atomic emission spectrometry.
Following this analysis, the results are reviewed for high concentrations of
bismuth, mercury, molybdenum, silver, and tungsten and diluted accordingly.
Samples meeting this criterion are then analysed by inductively coupled
plasma-mass spectrometry. Results are corrected for spectral interelement
interferences.
Four acid digestions can dissolve most minerals: however, although the term
"near total" is used, depending on the sample matrix, not all elements are
quantitatively extracted.
Results for the additional rare earth elements will represent the acid
leachable portion of the rare earth elements and as such, cannot be used, for
instance to do a chondrite plot.
Geochemical Procedure
Element geochemical procedure reporting units and limits are listed below:
Element Symbol Units Lower Limit Upper Limit
Aluminum Al % 0.01 50
Arsenic As ppm 0.2 10 000
Barium Ba ppm 10 10 000
Beryllium Be ppm 0.05 1 000
Bismuth Bi ppm 0.01 10 000
Calcium Ca % 0.01 50
Cadmium Cd ppm 0.02 1 000
Cerium Ce ppm 0.01 500
Cobalt Co ppm 0.1 10 000
Chromium Cr ppm 1 10 000
Cesium Cs ppm 0.05 500
Copper Cu ppm 0.2 10 000
Iron Fe % 0.01 50
Gallium Ga ppm 0.05 10 000
Germanium Ge ppm 0.05 500
Hafnium Hf ppm 0.1 500
Indium In ppm 0.005 500
Potassium K % 0.01 10
Lanthanum La ppm 0.5 10 000
Lithium Li ppm 0.2 10 000
Magnesium Mg % 0.01 50
Manganese Mn ppm 5 100 000
Element Symbol Units Lower Limit Upper Limit
Molybdenum Mo ppm 0.05 10 000
Sodium Na % 0.01 10
Niobium Nb ppm 0.1 500
Nickel Ni ppm 0.2 10 000
Phosphorous P ppm 10 10 000
Lead Pb ppm 0.5 10 000
Rubidium Rb ppm 0.1 10 000
Rhenium Re ppm 0.002 50
Sulphur S % 0.01 10
Antimony Sb ppm 0.05 10 000
Scandium Sc ppm 0.1 10 000
Selenium Se ppm 1 1 000
Tin Sn ppm 0.2 500
Strontium Sr ppm 0.2 10 000
Tantalum Ta ppm 0.05 100
Tellurium Te ppm 0.05 500
Thorium Th ppm 0.2 10 000
Titanium Ti % 0.005 10
Thallium Tl ppm 0.02 10 000
Uranium U ppm 0.1 10 000
Vanadium V ppm 1 10 000
Tungsten W ppm 0.1 10 000
Method ME-MS81
This method involves a lithium borate fusion prior to acid dissolution and
ICP- MS analysis provides the most quantitative analytical approach for a
broad suite of trace elements. Options for adding the whole rock elements
from an |CP - AES analysis on the same fusion, or base metals from a separate
four acid digestion, are available.
Lower and upper detection limits are given below:
Element Symbol Units Lower Limit Upper Limit
Yttrium Y ppm 0.1 500
Zinc Zn ppm 2 10 000
Zirconium Zr ppm 0.5 500
Dysprosium Dy ppm 0.05 1 000
Erbium Er ppm 0.03 1 000
Europium Eu ppm 0.03 1 000
Gadolinium Gd ppm 0.05 1 000
Holmium Ho ppm 0.01 1 000
Lutetium Lu ppm 0.01 1 000
Neodymium Nd ppm 0.1 1 000
Praseodymium Pr ppm 0.03 1 000
Samarium Sm ppm 0.03 1 000
Terbium Tb ppm 0.01 1 000
Thulium Tm ppm 0.01 1 000
Ytterbium Yb ppm 0.03 1 000
· Laboratory inserted standards, blanks and duplicates were
analysed per industry standard practice. There was no evidence of bias from
these results.
Verification of sampling and assaying
The verification of significant intersections by either independent or
alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data verification, data
storage (physical and electronic) protocols.
Discuss any adjustment to assay data.
· Two of the drillholes have been twinned, at Tors Tank where
TT_005DD was drilled next to TT_003RC.
· Conversion of elemental analysis (REE parts per million) to
stoichiometric oxide (REO parts per million) was undertaken by ROM geological
staff using the below element to stoichiometric oxide conversion factors
(https://www.jcu.edu.au/news/releases/2020/march/rare-earth-metals-an-untapped-resource
(https://www.jcu.edu.au/news/releases/2020/march/rare-earth-metals-an-untapped-resource)
)
Table C1-1: Element -Conversion Factor -Oxide Form
Ce 1.2284 CeO(2)
Dy 1.1477 Dy(2)O(3)
Er 1.1435 Er(2)O(3)
Eu 1.1579 Eu(2)O(3)
Gd 1.1526 Gd(2)O(3)
Ho 1.1455 Ho(2)O(3)
La 1.1728 La(2)O(3)
Lu 1.1371 Lu(2)O(3)
Nd 1.1664 Nd(2)O(3)
Pr 1.2083 Pr(6)O(11)
Sm 1.1596 Sm(2)O(3)
Tb 1.1762 Tb(4)O(7)
Tm 1.1421 Tm(2)O(3)
Y 1.2699 Y(2)O(3)
Yb 1.1387 Yb(2)O(3)
Rare earth oxide is the industry accepted form for reporting rare earths. The
following calculations are used for compiling REO into their reporting and
evaluation groups:
TREO (Total Rare Earth Oxide) = La(2)O(3) + CeO(2) + Pr(6)O(11) + Nd(2)O(3) +
Sm(2)O(3) + Eu(2)O(3) + Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3) + Ho(2)O(3) +
Er(2)O(3) + Tm(2)O(3) + Yb(2)O(3) + Y(2)O(3) + Lu(2)O(3).
TREO-Ce = TREO - CeO(2)
LREO (Light Rare Earth Oxide) = La(2)O(3) + CeO(2) + Pr(6)O(11) + Nd(2)O(3) +
Sm(2)O(3)
HREO (Heavy Rare Earth Oxide) = Eu(2)O(3) + Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3)
+ Ho(2)O(3) + Er(2)O(3) + Tm2O3 + Yb2O3 + Y2O3 + Lu2O3
CREO (Critical Rare Earth Oxide) = Nd(2)O(3) + Eu(2)O(3) + Tb(4)O(7) +
Dy(2)O(3) + Y(2)O(3)
MREO (Magnetic Rare Earth Oxide) = Pr(6)O(11) + Nd(2)O(3) + Sm(2)O(3) +
Gd(2)O(3) + Tb(4)O(7) + Dy(2)O(3).
Total Rare Earth Oxides (TREO):
To calculate TREO an oxide conversion "factor" is applied to each rare-earth
element assay. The "factor" equates an elemental assay to an oxide
concentration for each element. Below is an example of the factor calculation
for Lanthanum (La):
o Relative Atomic Mass (La) = 138.9055
o Relative Atomic Mass (O) = 15.9994
o Oxide Formula = La(2)O(3)
o Oxide Conversion Factor = 1/ ((2x 138.9055)/(2x 138.9055 + 3x 15.9994))
Oxide Conversion Factor = 1.173 (3dp)
None of the historical data has been adjusted.
Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and
down-hole surveys), trenches, mine workings and other locations used in
Mineral Resource estimation.
Specification of the grid system used.
Quality and adequacy of topographic control.
In general, locational accuracy does vary, depending upon whether the
historical surface and drillhole samples were digitised off plans or had their
coordinated tabulated. Many samples were originally reported to AGD66 or
AMG84 and have been converted to MGA94 (Zone 54)
The holes are currently surveyed with handheld GPS, awaiting more accurate
DGPS survey. It is thus estimated that locational accuracy therefore varies
between 2-4m until the more accurate surveying is completed. This assessment
was confirmed once the holes were surveyed by DGPS from GMC Surveying.
The quality of topographic control (GSNSW 1 sec DEM) is deemed adequate for
the purposes of the exploration drilling program.
Data spacing and distribution
Data spacing for reporting of Exploration Results.
Whether the data spacing and distribution is sufficient to establish the
degree of geological and grade continuity appropriate for the Mineral Resource
and Ore Reserve estimation procedure(s) and classifications applied.
Whether sample compositing has been applied.
The average sample spacing from the current drilling program across the tenure
varies per prospect, and sample type, as listed in Table C1-2, below:
Table C1-2: EL 8434 Drillhole Spacing
Prospect Drillholes Completed RMS Drillhole Spacing (m)
The Sisters Not yet
Iron Blow Not Yet
Tors Tank 4 127
Fence Gossan 4 208
Ziggy's Hill n/a n/a
Reefs Tank 4 221
The Datamine software allows creation of fixed length samples from the
original database given a set of stringent rules.
Sample location is shown in Figure C1.
Figure C1: Location of Stage 1 Fence Gossan Surface Samples
Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible
structures and the extent to which this is known, considering the deposit
type.
If the relationship between the drilling orientation and the orientation of
key mineralised structures is considered to have introduced a sampling bias,
this should be assessed and reported if material.
Historical drill holes at the BHAE are typically drilled vertically for auger
and RAB types (drilled along section lines) and angled at -55˚ or -60˚ to
the horizontal and drilled perpendicular to the mineralised trend for RC and
DDH.
Drilling orientations are adjusted along strike to accommodate folded
geological sequences. All Fence Gossan holes were designed to drill toward
grid south at an inclination of 60 degrees from horizontal.
The drilling orientation is not considered to have introduced a sampling bias
on assessment of the current geological interpretation.
Geological mapping by various companies has reinforced that the strata dips
variously between 5 and 65 degrees.
Sample security
The measures taken to ensure sample security.
Sample security procedures are considered 'industry standard' for the current
period.
Samples obtained during drilling completed between 4/10/22 to the 10/10/22
were transported by exploration employees or an independent courier directly
from Broken Hill to ALS Laboratory, Adelaide.
The Company considers that risks associated with sample security are limited
given the nature of the targeted mineralisation.
Audits or reviews
The results of any audits or reviews of sampling techniques and data.
No external audits or reviews have yet been undertaken.
SECTION 2: REPORTING OF EXPLORATION RESULTS
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status Type, reference name/number, location and ownership including agreements or EL 8434 is located about 28km east of Broken Hill whilst EL 8435 is 16km east
material issues with third parties such as joint ventures, partnerships, of Broken Hill. Both tenures are approximately 900km northwest of Sydney in
overriding royalties, native title interests, historical sites, wilderness or far western New South Wales (Figures C2-1 and C2-2 in Appendix A &B,
national park and environmental settings. above).
The security of the tenure held at the time of reporting along with any known EL 8434 and EL 8435 were both granted on the 2(nd of) June 2016 to Squadron
impediments to obtaining a licence to operate in the area. Resources for a term of five (5) years for Group One Minerals. On the 25(th
of) May 2020, Squadron Resources changed its name to Wyloo Metals Pty Ltd
(Wyloo). In December 2020 the tenure was transferred from Wyloo Metals to
Broken Hill Alliance Pty Ltd a 100% subsidiary company of Castillo Copper
Limited. Both tenures were renewed on the 12(th of) August 2021 for a
further six (6) years and are due to expire on the 2(nd of) June 2027.
EL 8434 lies across two (2) 1:100,000 geology map sheets Redan 7233 and
Taltingan 7234, and two (2) 1:250,000 geology map sheets, SI54-3 Menindee, and
SH54-15 Broken Hill in the county of Yancowinna. EL 8434 consists of one
hundred and eighty-six (186) units) in the Adelaide and Broken Hill
1:1,000,000 Blocks covering an area of approximately 580km(2).
EL 8435 is located on the 1:100,000 geology map sheet Taltingan 7234, and the
1:250,000 geology map sheet SH/54-15 Broken Hill in the county of
Yancowinna. EL 8435 consists of twenty-two (22) units (Table 1) in the
Broken Hill 1:1,000,000 Blocks covering an area of approximately 68km(2).
Access to the tenures from Broken Hill is via the sealed Barrier Highway.
This road runs north-east to south-west through the northern portion of the EL
8434, passes the southern tip of EL 8435 eastern section and through the
middle of the western section of EL 8435. Access is also available via the
Menindee Road which runs north-west to south-east through the southern section
of the EL 8434. The Orange to Broken Hill Rail line also dissects EL 8435
western section the middle and then travels north-west to south-east slicing
through the eastern arm of EL 8434 (Figure C2-1).
Figure C2-1: EL 8434 and EL 8435 General Location Map
Exploration done by other parties Acknowledgment and appraisal of exploration by other parties. Explorers who were actively involved over longer historical periods in various
parts of EL8434 were: - North Broken Hill Ltd, CRAE Exploration, Major Mining
Ltd and Broken Hill Metals NL, Pasminco Exploration Ltd, Normandy Exploration
Ltd, PlatSearch NL/Inco Ltd/ EGC Pty Ltd JV and the Western Plains Gold
Ltd/PlatSearch/EGC Pty Ltd JV.
A comprehensive summary of work by previous explorers was presented in Leyh
(2009). However, more recently, follow-up field reconnaissance of areas of
geological interest, including most of the prospective zones was carried out
by EGC Pty Ltd over the various licenses. This work, in conjunction with a
detailed interpretation of aeromagnetic, gravity plus RAB / RC drill hole
logging originally led to the identification of at least sixteen higher
priority prospect areas. All these prospects were summarized in considerable
detail in Leyh (2008). Future work programs were then also proposed for each
area. Since then, further compilation work plus detailed geological
reconnaissance mapping and sampling of gossans and lode rocks has been carried
out.
A total of 22 prospects were then recognised on the exploration licence with
at least 12 occurring in and around the tenure.
With less than 45% outcropping Proterozoic terrain within the licence, this
makes it very difficult to explore and is in the main very effectively
screened from the easy application of more conventional exploration
methodologies due to a predominance of extensive Cainozoic cover sequences.
These include recent to young Quaternary soils, sands, clays and older more
resistant, only partially dissected, Tertiary duricrust regolith covered
areas. Depth of cover ranges from a few metres in the north to over 60
metres in some areas on the southern and central license.
Exploration by EGC Pty Ltd carried out in the field in the first instance has
therefore been heavily reliant upon time consuming systematic geological
reconnaissance mapping and relatable geochemical sampling. These involve a
slow systematic search over low outcropping areas, poorly exposed subcrops and
float areas as well as the progressive development of effective regolith
mapping and sampling tools. This work has been combined with a vast amount
of intermittently acquired past exploration data. The recent data
compilation includes an insufficiently detailed NSWGS regional mapping scale
given the problems involved, plus some regionally extensive, highly variable,
low-level stream and soil BLEG geochemical data sets over much of the area.
There are also a few useful local detailed mapping grids at the higher
priority prospects, and many more numerous widespread regional augers, RAB,
and percussion grid drilling data sets. Geophysical data sets including ground
magnetics, IP and EM over some prospect areas have also been integrated into
the exploration models. These are located mainly in former areas of moderate
interest and most of the electrical survey methods to date in this type of
terrain continue to be of limited application due to the high degree of
weathering and the often prevailing and complex regolith cover constraints.
Between 2007 and 2014 Eaglehawk Geological Consulting has carried out detailed
research, plus compilation and interpretation of a very large volume of
historic exploration data sourced from numerous previous explorers and dating
back to the early 1970's. Most of this data is in non-digital scanned form.
Many hard copy exploration reports (see references) plus several hundred plans
have been acquired from various sources, hard copy printed as well as
downloaded as scans from the Geological Survey of NSW DIGS system. They also
conducted field mapping, costean mapping and sampling, and rock chip sampling
and analysis.
Work Carried out by Squadron Resources and Whyloo Metals 2016-2020
Research during Year 1 by Squadron Resources revealed that the PGE-rich,
sulphide-bearing ultramafic rocks in the Broken Hill region have a
demonstrably alkaline affinity. This indicates a poor prospectivity for
economic accumulations of sulphide on an empirical basis (e.g., in comparison
to all known economic magmatic nickel sulphide deposits, which have a
dominantly tholeiitic affinity). Squadron instead directed efforts toward
detecting new Broken Hill-Type (BHT) deposits that are synchronous with basin
formation. Supporting this modified exploration rationale are the EL's
stratigraphic position, proximity to the Broken Hill line of lode, abundant
mapped alteration (e.g., gahnite and/or garnet bearing exhalative units) and
known occurrences such as the "Sisters" and "Iron Blow" prospects.
The area overlies a potential magmatic Ni-Cu-PGE source region of
metasomatised sub-continental lithospheric mantle (SCLM) identified from a
regional targeting geophysical data base. The exploration model at the time
proposed involved remobilization of Ni-Cu-PGE in SCLM and incorporation into
low degree mafic-ultramafic partial melts during a post-Paleoproterozoic plume
event and emplacement higher in the crust as chonoliths/small intrusives -
Voisey's Bay type model. Programs were devised to use geophysics and
geological mapping to locate secondary structures likely to control and
localise emplacement of Ni-Cu-PGE bearing chonoliths. Since EL8434 was
granted, the following has been completed:
• Airborne EM survey.
• Soil and chip sampling.
• Data compilation.
• Geological and logistical reconnaissance.
• Community consultations; and
• Execution of land access agreements.
Airborne EM Survey
Geotech Airborne Limited was engaged to conduct an airborne EM survey using
their proprietary VTEM system in 2017. A total of 648.92-line kilometres
were flown on a nominal 200m line spacing over a portion of the project area.
Several areas were infilled to 100m line spacing.
The VTEM data was interpreted by Southern Geoscience Consultants Pty Ltd, who
identified a series of anomalies, which were classified as high or low
priority based on anomaly strength (i.e., does the anomaly persist into the
latest channels). Additionally, a cluster of VTEM anomalies at the "Sisters"
prospect have been classified separate due to strong IP effects observed in
the data. Geotech Airborne have provided an IP corrected data and
interpretation of the data has since been undertaken.
Soil and Chip sampling
The VTEM anomalies were followed up by a reconnaissance soil sampling
programme. Spatially clustered VTEM anomalies were grouped, and follow-up soil
lines were designed. Two (2) VTEM anomalies were found to be related to
culture and consequently no soils were collected. Two (2) other anomalies
were sampled which were located above thick alluvium of Stephens Creek and
were therefore not sampled. A line of soil samples was collected over a
relatively undisturbed section at Iron Blow workings and the Sisters Prospect.
One hundred and sixty-six (166) soil samples were collected at a nominal 20cm
depth using a 2mm aluminum sieve. Two (2) rock chips were also collected
during this program. The samples were collected at either 20m or 40m spacing
over selected VTEM anomalies. The samples were pulverised and analysed by
portal XRF at ALS laboratories in Perth.
Each site was annotated with a "Regolith Regime" such that samples from a
depositional environment could be distinguished from those on exposed
Proterozoic bedrock, which were classified as an erosional environment. The
Regolith Regime groups were used for statistical analysis and levelling of the
results. The levelled data reveals strong relative anomalies in zinc at VTEM
anomaly clusters 10, 12 and 14 plus strong anomalous copper at VTEM 17.
Geology Deposit type, geological setting, and style of mineralisation. As the strata is tightly folded, the intersected cobalt-rich layers are
overstated in terms of apparent thickness, however the modelling software
calculates a true, vertical thickness. Cobalt mineralisation is commonly
associated with shears, faults, amphibolites, and a quartz-magnetite rock
within the shears, or on or adjacent to the boundaries of the Himalaya
Formation. In general, most of the cobalt and rare earth element - rich layers
have a north-northwest to north strike.
REE enrichment generally occurs as a 5 to 10-metre-thick zone between the
completely weathered layer and strongly weathered layer and it is targeted for
commercial mining (Figure D2-2). Compared to other REE deposits,
regolith-hosted rare earth element deposits are substantially low-moderate
grade (containing 0.05-0.3 wt.% extractable REEs). Nevertheless, due to its
easy extraction method, low processing costs and large abundance, the
orebodies are generally economic to be extracted (Duuring, (2020); Kanazawa
and Kamitani (2006); and Murakami, H.; Ishihara (2008)).
Figure C2-2: Weathering Profile over REE - Rich Granite
https://en.wikipedia.org/wiki/Regolith-hosted_rare_earth_element_deposits
(https://en.wikipedia.org/wiki/Regolith-hosted_rare_earth_element_deposits)
Weathering profile of regolith hosted REE deposits shown above, the legend is:
(A) Humic layer. (B) Completely weathered layer. (C) Strongly weathered layer.
(D) Weathering front. (E) Unweathered rock.
Most of the REE found in cerium monazite (Ce (PO(4))) which always contains
major to minor amounts of other REE (Nd, La, Pr, Sm etc) replacing Ce. Also,
the mineral often contains trace amounts of U and Th (coupled with Ca). This
will be collaborated with XRD and or SEM analysis.
Drill hole Information A summary of all information material to the understanding of the exploration Header information about all drillholes and surface samples completed at Tors
results including a tabulation of the following information for all Material Tank and Fence Gossan have been tabulated in this release in Appendix B.
drill holes:
o easting and northing of the drill hole collar
o elevation or RL (Reduced Level - elevation above sea level in metres) of
the drill hole collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
If the exclusion of this information is justified on the basis that the
information is not Material and this exclusion does not detract from the
understanding of the report, the Competent Person should clearly explain why
this is the case.
Data aggregation methods In reporting Exploration Results, weighting averaging techniques, maximum No metal equivalents have been reported. Rare earth element results have
and/or minimum grade truncations (e.g., cutting of high grades) and cut-off been converted to rare earth oxides as per standard industry practice
grades are usually Material and should be stated. (Castillo Copper 2022f).
Where aggregate intercepts incorporate short lengths of high-grade results and No compositing of assay results has taken place, but rather menu options
longer lengths of low-grade results, the procedure used for such aggregation within the Datamine GDB module have been used to create fixed length 1m assay
should be stated and some typical examples of such aggregations should be intervals from the original sampling lengths.
shown in detail.
The rules follow very similarly to those used by the Leapfrog Geo software in
The assumptions used for any reporting of metal equivalent values should be creating fixed length samples.
clearly stated.
Relationship between mineralisation widths and intercept lengths These relationships are particularly important in the reporting of Exploration A database of all the historical borehole sampling has been compiled and
Results. validated. It is uncertain if there is a strong relationship between the
surface sample anomalies to any subsurface anomalous intersections due to the
If the geometry of the mineralisation with respect to the drill hole angle is possible masking by variable Quaternary and Tertiary overburden that varies in
known, its nature should be reported. depth from 0-15m. The mineralisation appears to be secondary enrichment in
the regolith clays and extremely weathered material derived from
If it is not known and only the down hole lengths are reported, there should quartzo-feldspathic pegmatites.
be a clear statement to this effect (e.g., 'down hole length, true width not
known').
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts Current surface anomalies are shown on maps released on the ASX (Castillo
should be included for any significant discovery being reported These should Copper 2022d, 2022e, 2022f and 2022g). All historical surface sampling has
include, but not be limited to a plan view of drill hole collar locations and had their coordinates converted to MGA94, Zone 54.
appropriate sectional views.
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable, All recent laboratory analytical results have been recently reported (see
representative reporting of both low and high grades and/or widths should be Castillo Copper 2022a, b, c, d, e, f, and g) for assay results.
practiced to avoid misleading reporting of Exploration Results.
Regarding the surface and sampling, no results other than duplicates, blanks
or reference standard assays have been omitted.
Other substantive exploration data Other exploration data, if meaningful and material, should be reported Historical explorers have also conducted airborne and ground gravity,
including (but not limited to): geological observations; geophysical survey magnetic, EM, and IP resistivity surveys over parts of the tenure area but
results; geochemical survey results; bulk samples - size and method of this is yet to be fully georeferenced (especially the ground IP surveys).
treatment; metallurgical test results; bulk density, groundwater, geotechnical Squadron Resources conducted an airborne EM survey in 2017 that covers Iron
and rock characteristics; potential deleterious or contaminating substances. Blow and The Sisters, but not the southern cobalt and REE prospects.
Further work The nature and scale of planned further work (e.g., tests for lateral It is recommended that:
extensions or depth extensions or large-scale step-out drilling).
· Complete rehabilitation of the 2022 BHAE drilling campaign that
Diagrams clearly highlighting the areas of possible extensions, including the comprised mostly RC drilling. An application supporting an ESF2 lodgment
main geological interpretations and future drilling areas, provided this is yet to be approved by the NSW Resource Regulator
information is not commercially sensitive.
· The remaining non-sampled zones within the Core Library
drillholes, BH1, BH2, and DD90-IB3 in the north of the tenure group be
relogged and sampled. DD90-IB3 had 21-87m retested recently and is a good
candidate for hyperspectral logging.
· A program of field mapping and ground magnetic, IP or radiometric
surveys be planned and executed at Fence Gossan. Mapping of pegmatite
outcrops is a high priority.
· Generate an Exploration Target for Fence Gossan to the standard
of Clause 17 of the 2012 JORC Code.
· Depending upon the results of the proposed geophysical surveys
and Exploration Target noted above, the next drilling program will
specifically target the air coring technique over the known cobalt and REE
mineralisation downdip to at least 30m depth at all three prospects. That
proposed drilling program is also designed to increase the resource confidence
of the REE to Inferred Resources to the standard of the 2012 JORC Code.
REFERENCES
Biggs, M. S., 2021a, Broken Hill Alliance, NSW Tenure Package Background
Geological Information, unpublished report to BH Alliance Pty Ltd, Sep 21,
30pp.
Biggs, M. S., 2021b, EL 8434 and EL 8435, Brief Review of Surface Sample
Anomalies Lithium, Rare Earth Elements and Cobalt, unpublished report to BH
Alliance Pty Ltd, Nov 21, 18pp.
Biggs, M.S., 2022a, BHA Cobalt Modelling and Mineral Resource Estimate Update,
unpublished memo for Castillo Copper by ROM Resources.
Biggs, M.S., 2022b, Broken Hill BHA Tenures Update, Castillo Copper,
unpublished memo prepared by ROM Resources, Mar 22, 5pp.
Biggs M.S., 2022c, Geological Briefing Paper, Iron Blow Prospect, East Zone,
BHA Project (BHAE), Broken Hill, NSW, ROM Resources, prepared for Castillo
Copper Limited, August 2022
Burkett R.D., 1975, Progress Report on Exploration Licenses 780, 781, 782 and
783, Broken Hill Area, NSW for the six months to 23rd November 1975, North
Broken Hill Limited for the NSW Geological Survey, (GS1975-328)
Castillo Copper Limited, 2020, ASX Release Acquisition enhances BHT
(zinc-silver-lead) and IOCG (gold-copper) prospectivity at Broken Hill, 1st
October 2020.
Castillo Copper Limited, 2022a, ASX Release Battery metal drill-hole assays
unlock BHA East Zone potential / lithium update, 5th January 2022.
Castillo Copper Limited, 2022b, ASX Release Strategic focus to develop
significant cobalt mineralisation potential at BHA Project, 9th February 2022.
Castillo Copper Limited, 2022c, ASX Release High grade platinum confirmed at
BHA Project, 9th March 2022.
Castillo Copper Limited, 2022d ASX Release Diamond core tests demonstrate
high-grade cobalt-zinc potential at Broken Hill, 21 March 2022
Castillo Copper Limited, 2022e ASX Release, Drilling hits targeted cobalt
zones & wide pegmatite intercepts at Broken Hill 12 October 2022
Castillo Copper Limited, 2022f ASX Release, Drilling hits more wide pegmatite
intercepts at Broken Hill, 24 October 2022
Castillo Copper Limited, 2022g ASX Release, Completed auger sampling campaign
targets 6.5km(2) REE mineralisation zone, 23 December 2022
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-Yellowstone Area, Broken Hill, New South Wales for the six months period
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ended 29th December 1976, North Broken Hill Limited, Report GS1976-198, Feb
1977, 24pp.
Leyh W.R., 1977b, Progress Report on Farmcote Exploration Licenses 780 and
782, Farmcote Area, Broken Hill, NSW for the three months to 5th March 1977,
North Broken Hill Limited for the NSW Geological Survey, (GS1977-078)
Leyh W.R., 1977c, Progress Report on Farmcote Exploration Licenses 780 and
782, Farmcote Area, Broken Hill, NSW for the three months to 23rd May 1977,
North Broken Hill Limited for the NSW Geological Survey, (GS1977-078)
Leyh W.R., 1978, Progress Report on Farmcote Exploration Licenses 780 and 782,
Farmcote Area, Broken Hill, NSW for the three months to 27 October 1978, North
Broken Hill Limited for the NSW Geological Survey, (GS1977-078)
Leyh W.R., 1978 Progress Report on Exploration Licenses 1099 and 1100 for the
six months to 27 October 1978, North Broken Hill Limited for the NSW
Geological Survey, (GS1978-407).
Leyh, W.R., 1990, Exploration Report for the Third Six Monthly Period ended
12th June 1990 for EL 3238 (K Tank), Broken Hill District, New South Wales for
the six months period, Pasminco Limited, Report GS1989-226, Jun 90, 22pp.
Leyh, W.R., and Lees T.C., 1977, Progress Report on Exploration Licence, No.
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months period ended 29th June 1977, North Broken Hill Limited, Report
GS1976-198, Jul 77, 35pp.
Leyh, W.R., and Larson P.D., 1981, Final Report for the Third Six Monthly
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Jun 90, 22pp.
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19/2/1997, Normandy Exploration Limited, unpublished report to the GSNSW, RIN
00002672
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November 1980 to 7th May 1981, EL 1106 Rockwell, Broken Hill, NSW, CRA
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