REG - Cobra Resources PLC - Wudinna Project Update
07/02/2022 07:00
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RNS Number : 7923A Cobra Resources PLC 07 February 2022
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7 February 2022
Cobra Resources plc
("Cobra" or the "Company")
Wudinna Project Update
Northern Drillholes at Clarke Intercept Additional Gold Mineralisation
Additional Rare Earth Interceptions Directly Above Gold Zones
Cobra, a gold exploration company focused on the Wudinna Gold Project in South
Australia, announces additional results from the Company's recent 14-hole
phase of Reverse Circulation ("RC") drilling on the Clarke prospect. The
Company is pleased to report:
· Further gold mineralisation has been intercepted within the northern
drill transect confirming the potential for a significant gold mineral system
at Clarke
· Additional Rare Earth Elements ("REE") have been intercepted above
and proximal to gold interceptions. The Board considers the discovery of
critical REEs overlaying gold mineralisation to be significant, with grades
and intercept widths (summarised further below) comparable to other rare earth
projects of considerable market value. This discovery now exposes Cobra to
multiple high value commodities
Fire assay results for gold have now been received for all holes in the recent
phase of drilling on the Clarke prospect, multi-element and rare earth results
are outstanding for a single hole.
Rupert Verco, CEO of Cobra, commented:
"The results of the programme have demonstrated that the gold system at Clarke
is considerable in size, open to the north and continues to present as a
compelling target to add further ounces to the existing Mineral Resource
Estimate.
The rare earth discovery is also proving to be significant. The occurrence of
rare earths above defined gold mineralisation makes the discovery unique when
compared to other rare earth projects. We have work to do to define the extent
of this discovery and to understand its potential to contribute to future
project economics, but undoubtedly this has added a new and very interesting
dimension to Cobra's potential.
There is a growing demand for magnet rare earths and an upward forecast in
pricing. A vertically associated gold and clay hosted rare earth deposit
offers shareholders exposure to multiple high value and high demand
commodities in close spatial proximity. We look forward to growing a mineral
resource that places Cobra in an exclusive position within the mineral
resource sector.
We are in the process of interpreting results and finalising our planned 2022
work programme that will focus on increasing our current gold resource,
increasing the footprint of rare earth mineralisation, and drill testing our
IOCG targets."
A presentation of results from the 2021 drilling programme of the Clarke
prospect with management commentary is available to view on the Company's
website at www.cobraplc.com/category/presentations/
(http://www.cobraplc.com/category/presentations/) .
Highlights:
· CBRC0050 intercepted 33m at 1.03 g/t gold from 65m, including 9m at
2.09 g/t gold from 65m(1)
· Gold mineralisation has now been intercepted over 400m of strike at
Clarke with mineralisation open to the northwest of CBRC0050
· All holes intercepted rare earth mineralisation within the saprolite
zone, where:
o The average true width of mineralisation is 18.7m and the average Total
Rare Earth Oxides ("TREO") is 597 ppm(2)
o High-grade intervals exist within the intercepts, where drillhole
CBRC0044 intercepted a true width of 9.4m at 1,030 ppm TREO, CBRC0043
intercepted a true width of 4.7m at 1,160 ppm TREO and CBRC0054 intercepted 6m
at 1,446 ppm TREO
o The highest 1m intercept grade was 9,024 ppm TREO in CBRC0048
o Intercepts are enriched in high value rare earths where neodymium/
praseodymium equate to 21.5% of the TREO and dysprosium equates to 2.2%
· Rare earth mineralisation intercepts are low in uranium (6 ppm
average) and thorium (28 ppm average), a favourable attribute of Ion Adsorbed
Clay ("IAC") rare earth deposits
· Results support the likelihood of rare earths overlaying gold
mineralisation at Barns and Baggy Green as well
· Preliminary results from X-ray diffraction ("XRD") performed by the
Commonwealth Scientific and Industrial Research Organisation ("CSIRO")
demonstrates that mineralisation is supportive of REEs being adsorbed to clay
mineralogy
The discovery of critical REEs overlaying gold mineralisation at Clarke is
significant, with grades and intercept widths comparable to other IAC hosted
rare earth projects of considerable market value
· Rare earth mineralisation is open to the north, south, east, and west
of current drilling
· REE intercepts confirmed above previously reported gold
intercepts(3), including:
o CBRC0042 intercepted 8.2m at 561 ppm TREO from 38.1m below surface,
which is above the previously reported 19m at 0.79 g/t gold from 83m,
including 5m at 2.62 g/t gold from 95m
o CBRC0043 intercepted 19.7m at 569 ppm TREO from 31m below surface,
including 4.7m at 1,160 ppm TREO from 38.5m below surface. This is in
association with the 96m at 0.55 g/t gold from 30m, including 20m at 1.5 g/t
gold from 88m
o CBRC0044 intercepted 19.7m at 717 ppm TREO from 31m, including 9.4m at
1030 ppm TREO from 33m
o CBRC0050 intercepted 4.7m at 380 ppm TREO from 15m and 3.8m at 456 ppm
TREO from 48m below surface. This is above the 33m at 1.03 g/t gold from 65m,
including 9m at 2.09 g/t
· Additional rare earth results proximal to gold mineralisation at
Clarke include:
o CBRC0046 intercepted 40.4m at 669 ppm TREO from 19.7m, including 14.1m
at 852 ppm TREO from 19.7m and 9.4m at 830 ppm TREO from 47.9m
o CBRC0048 intercepted 34.8m at 629 ppm TREO from 18.8m, including 0.9m at
9,024 ppm TREO
o CBRC0045 intercepted 22.6m at 638 ppm TREO from 31m, including 2.8m at
993 ppm TREO, 1.9m at 1,972 ppm TREO and 2.8m at 1,053 ppm TREO
o CBRC0047 intercepted 9.4m at 682 ppm TREO from 18.8m, including 2.8m at
1,322 ppm TREO
o CBRC0051 intercepted 7.5m at 783 ppm TREO from 14.1m, including 1.9m at
1,447 ppm TREO
o CBRC0052 intercepted 22.6m at 435 ppm TREO from 16.9m below surface
o CBRC0054 intercepted 16m at 920 ppm TREO from 16.9m below surface,
including 5.6m at 1,446 ppm TREO
(1) Gold results reported as downhole intercepts
(2) Reported using Datamine true width calculator
(3) Rare earth results reported as true width intercepts
In addition to this release, a version of this report with supplementary
information and images can be found at
http://www.rns-pdf.londonstockexchange.com/rns/7923A_1-2022-2-4.pdf
(http://www.rns-pdf.londonstockexchange.com/rns/7923A_1-2022-2-4.pdf)
Enquiries:
Cobra Resources plc via Vigo Consulting
Rupert Verco (Australia) +44 (0)20 7390 0234
Dan Maling (UK)
SI Capital Limited (Joint Broker) +44 (0)1483 413 500
Nick Emerson
Sam Lomanto
Peterhouse Capital Limited (Joint Broker) +44 (0)20 7469 0932
Duncan Vasey
Lucy Williams
Vigo Consulting (Financial Public Relations) +44 (0)20 7390 0234
Ben Simons
Charlie Neish
Kendall Hill
The person who arranged for the release of this announcement was Rupert Verco,
CEO of the Company.
About Cobra
Cobra's Wudinna Gold Project is located in the Gawler Craton which is home to
some of the largest IOCG discoveries in Australia including Olympic Dam, as
well as Prominent Hill and Carrapateena. Cobra's Wudinna tenements contain
extensive orogenic gold mineralisation and are characterised by potentially
open-pitable, high-grade gold intersections, with ready access to nearby
infrastructure. In total Cobra has over 22 orogenic gold prospects, with
grades of between 16 g/t up to 37.4 g/t gold outside of the current 211,000 oz
JORC Mineral Resource Estimate, as well as one copper-gold prospect, and five
IOCG targets.
Wudinna Project Description
The Eyre Peninsula Gold Joint Venture comprises a 1,928 km(2) land holding in
the Gawler Craton. The Wudinna Gold Project within the Joint Venture tenement
holding comprises a cluster of gold prospects which includes the Barns, White
Tank and Baggy Green deposits.
Competent Persons Statement
Information and data presented within this announcement has been compiled by
Mr Robert Blythman, a Member of the Australian Institute of Geoscientists
("MAIG"). Mr Blythman is a Consultant to Cobra Resources Plc and has
sufficient experience, which is relevant to the style of mineralisation,
deposit type and to the activity which he is undertaking to qualify as a
Competent Person defined by the 2012 Edition of the Australasian Code for
Reporting Exploration Results, Mineral Resources and Ore Reserves (the "JORC"
Code). This includes 10 years of Mining, Resource Estimation and Exploration
relevant to the style of mineralisation.
Information in this announcement has been assessed by Mr Rupert Verco, a
Fellow of the Australasian Institute of Mining and Metallurgy ("FAusIMM"). Mr
Verco an employee of Cobra Resources Plc has more than 15 years relevant
industry experience, which is relevant to the style of mineralisation, deposit
type and to the activity which he is undertaking to qualify as a Competent
Person as defined in the 2012 Edition of the Australasian Code for Reporting
Exploration Results, Mineral Resources and Ore Reserves (the "JORC" Code).
This includes 10 years of Mining, Resource Estimation and Exploration relevant
to the style of mineralisation.
Information in this announcement relates to exploration results that have been
reported in the following announcements:
"Wudinna Project Update - Initial Gold and Rare Earth Results", dated 14
December 2021
"Wudinna Project Update - Clarke Gold Assay Results", dated 3 December 2020
Further information on the Clarke drilling programme
The Clarke gold and REE prospect is located 1.75 km north of the 94,000 oz
Baggy Green deposit that forms part of the Wudinna Project's 211,000 oz
Mineral Resource Estimate. In Cobra Resources' maiden 2020 drilling programme,
drilling intercepted 31m at 3.06 g/t to the north of previously intercepted
gold mineralisation at the Clarke prospect.
Follow-up pathfinder drilling in 2021 defined a zone of anomalous gold and
associated pathfinder elements across a 1.1 km zone at Clarke. In November
2021, the Company completed a 14-hole (2,144m) RC programme that was designed
to test the extent of the anomaly and the northern continuity of previously
defined gold mineralisation.
Re-analysis of samples from drillhole CBRC0009 confirmed the presence of
elevated rare earths within the weathered kaolinised clays that lie directly
above intercepted gold mineralisation. This confirmed the requirement to
perform additional rare earth analysis within the weathered saprolite zone.
Significant intercepts from the programme include:
Table 1: Significant gold intercepts form the 2021 exploration programme,
reported as downhole intercepts
Hole ID From To Interval Au (g/t) Including
CBRC0050 65 98 33 1.03 Including 9m @ 2.09 g/t Au 65-75m
CBRC0043 30 126 96 0.55 Including 8m at 0.61 g/t Au 32-40m
Including 20m at 1.5 g/t Au 88-108m
Including 10m at 0.92 g/t Au 114-124m
CBRC0042 83 102 19 0.79 Including 5m at 2.65 g/t Au 83-87m
CBRC0044 109 118 9 0.23
Table 2: Significant rare earth oxide intercepts, reported as downhole and
true width
Hole ID DH From (m) DH To (m) DH Intercept (m) Depth From Surface True Width (m) TREO (ppm) Praseodymium Neodymium Terbium Dysprosium
Pr6O11 Nd2O3 Tb4O7 Dy
2O
3
ppm % TREO ppm % TREO ppm % TREO ppm % TREO
CBRC0042 42 51 9 38.1 8.2 561 25 4.4% 92 16.4% 2 0.3% 10 1.8%
CBRC0043 35 54 19 32.9 17.9 603 30 4.9% 107 17.7% 2 0.4% 14 2.4%
Inc 41 46 5 38.5 4.7 1,296 76 5.9% 277 21.4% 6 0.5% 35 2.7%
CBRC0044 33 54 21 31.0 19.7 717 35 4.9% 129 18.0% 3 0.4% 16 2.3%
Inc 35 45 10 32.9 9.4 1030 56 5.4% 202 19.7% 4 0.4% 25 2.4%
CBRC0045 33 57 24 31.0 22.6 638 25 3.9% 95 14.9% 3 0.4% 16 2.6%
Inc 33 36 3 31.0 2.8 993 33 3.4% 125 12.5% 3 0.3% 16 1.6%
Inc 39 41 2 36.6 1.9 1972 108 5.5% 400 20.3% 10 0.5% 51 2.6%
Inc 54 57 3 50.7 2.8 1053 26 2.5% 114 10.9% 6 0.6% 43 4.1%
CBRC0046 21 64 43 19.7 40.4 669 31 4.7% 113 16.9% 2 0.3% 13 2.0%
Inc 21 36 15 19.7 14.1 852 45 5.2% 160 18.8% 3 0.3% 16 1.9%
Inc 51 61 10 47.9 9.4 830 34 4.0% 124 15.0% 3 0.3% 16 2.0%
CBRC0047 20 30 10 18.8 9.4 682 36 5.2% 127 18.6% 3 0.4% 17 2.5%
Inc 25 28 3 23.5 2.8 1322 68 5.2% 246 18.6% 6 0.5% 37 2.8%
CBRC0048 20 57 37 18.8 34.8 629 35 5.6% 120 19.1% 3 0.5% 17 2.7%
Inc 20 21 1 18.8 0.9 9024 688 7.6% 2293 25.4% 52 0.6% 277 3.1%
CBRC0049 17 27 10 16.0 9.4 513 23 4.5% 83 16.2% 2 0.4% 12 2.3%
CBRC0050 16 21 5 15.0 4.7 380 16 4.2% 57 14.9% 1 0.3% 6 1.6%
CBRC0050 51 55 4 47.9 3.8 456 20 4.4% 71 15.6% 1 0.3% 7 1.5%
CBRC0051 15 23 8 14.1 7.5 783.2 35 4.4% 117 15.0% 3 0.3% 15 2.0%
Inc 19 21 2 17.9 1.9 1447 61 4.2% 207 14.3% 5 0.3% 29 2.0%
CBRC0052 18 42 24 16.9 22.6 435.2 18 4.1% 65 15.0% 2 0.4% 9 2.2%
CBRC0053 13 25 12 11.8 10.9 413 19 4.5% 67 16.2% 1 0.3% 7 1.7%
CBRC0054 18 35 17 16.9 16.0 920.1 40 4.4% 139 15.1% 3 0.3% 15 1.7%
Inc 22 28 6 20.7 5.6 1446 67 4.7% 238 16.5% 5 0.3% 26 1.8%
CBRC0009(1) 30 50 20 29.5 19.7 550 28 5.0% 101 18.3% 2 0.4% 13 2.3%
Inc 31 39 8 30.5 7.9 875 48 5.5% 176 20.1% 4 0.4% 21 2.4%
(1) Drilled in 2020, re-analysed for REEs and reported in Dec 2021
Results of the programme demonstrate:
· The strike of gold mineralisation at Clarke has been doubled, where
the extent of mineralisation now exceeds 400m
· Mineralisation is open to the northeast of drillhole CBRC0050 that
intersected 33m at 1.03 g/t
· The depth of gold mineralisation remains untested and is open with
depth
· The discontinuity of mineralisation across the central transect is
interpreted to be attributed to a late-stage E-W fault. The presence of which
has been supported by several geological indicators (refer to figure 1)
· HyLogger data demonstrates critical changes in mineralogical
composition associated with gold mineralisation that are considered critical
for future exploration targeting
· Rare earth minerals are accumulated within the kaolinised clays of
the saprolite (weathered) horizon. The intercept widths and grades are
comparable to other IAC projects and are considered economically beneficial to
the Wudinna project
· The Clarke drilling programme is the first that has identified rare
earth mineralisation, the potential extent of rare earths is potentially
significant due to:
o The margin settings of enriched Hiltaba Suite and Sleaford Complex
granites are present throughout the project's land tenure
o The depth extent of basement weathering, where kaolinised profiles of up
to 60m present as highly favourable zones to host IAC style rare earth
mineralisation
· Elevated rare earth grades have a spatial association to gold
mineralisation at Clarke and the saprolite weathering profile at Clarke
exhibits geological similarities to the saprolite horizons at Baggy Green and
Barns. Re-analysis of retained drillhole pulp samples presents as a low-cost
exploration opportunity to define further rare earth mineralisation
The proximity of rare earths to gold mineralisation is unique, the
complementary nature of both forms of mineralisation has the potential for
favourable economics: there are currently no IAC rare earth operating mines in
Australia, and no IAC rare earth projects with associated gold mineralisation
· Rare earth mineralisation is open in all directions and the
continuity and consistency of rare earth mineralisation means that there is a
significant opportunity to increase the extent of the current mineralisation
footprint
Rare earth results remain outstanding for hole CBRC0055. These results are
expected within two weeks. Results have been delayed due to the current
Covid-19 situation in South Australia.
Table 3: Drillhole collar details for all drillholes reported and results that
remain outstanding
Hole ID Easting Northing RL Depth Dip Azimuth Assays Received/ Reported
Au Multi Element Lanthanide
CBRC0009 547,047 6,364,928 105.9 123 -80 180 P P P
CBRC0042 546,945 6,364,933 105.6 162 -65 60 P Y Y
CBRC0043 547,065 6,364,940 105.6 126 -70 240 P Y Y
CBRC0044 547,107 6,364,965 104.9 190 -70 240 P Y Y
CBRC0045 547,151 6,364,992 104.7 138 -70 240 P Y Y
CBRC0046 546,903 6,364,963 104.8 156 -70 240 P Y Y
CBRC0047 546,993 6,365,014 106.2 138 -70 240 Y Y Y
CBRC0048 547,025 6,365,037 106.1 144 -70 240 Y Y Y
CBRC0049 547,080 6,365,065 104.3 144 -70 240 Y Y Y
CBRC0050 546,942 6,365,104 104.1 156 -70 240 Y Y Y
CBRC0051 546,985 6,365,128 104.3 156 -70 240 Y Y Y
CBRC0052 547,028 6,365,152 105.2 160 -70 240 Y Y Y
CBRC0053 546,906 6,364,667 107.1 150 -65 240 Y Y Y
CBRC0054 547,356 6,364,707 109.6 162 -70 240 Y Y Y
CBRC0055 547,311 6,364,682 108.4 162 -65 240 Y X X
P - Previously reported, Y - Received, X - Assays outstanding
HyLogger Analysis
Preliminary results from the South Australian Department of Mining HyLogger
analysis of drill chips have defined key alteration assemblages. Results
demonstrate chemical changes within key alteration mineral assemblages
directly associated with gold mineralisation that have previously been
unidentified. This is considered critical in understanding the nature of
mineralisation and will improve exploration targeting moving forward and
enable the development of robust geological models.
CSIRO Analysis
Preliminary XRD analyses from the CSIRO - Mineral Resources, supports that a
considerable portion of REOs are adsorbed to clay particles. This is from XRD
analyses of sieved samples >2 µm (microns) and <2 µm, where:
o Phosphorus pentoxide concentrations remained equal in both size fractions
(a compounding XRD analysis demonstrating negligible change in florencite and
monazite concentrations)
o The concentration of REEs effectively doubled in the fine (<2 µm)
fraction, indicating that REE bursary may be adsorbed to clay mineralogy
Next Steps
Analysis of HyLogger data and multi-element chemistry is underway to validate
the structural interpretation of the gold mineralisation at Clarke. Pending
findings, the decision to estimate a maiden gold mineral resource estimate at
Clarke before further drilling will be evaluated from the increased geological
understanding.
Further samples are at the CSIRO laboratories, Adelaide, to increase the
dataset and confirm the mineralogy of rare earths. Once these results are
received further testwork will commence to define the metallurgical
leachability.
Work is underway to identify samples from historic drillholes for re-analysis
that will focus on growing the footprint of rare earth mineralisation across
existing gold resources at Barns, White Tank and Baggy Green.
Further detail regarding the Company's planned 2022 exploration works
programme will be made available in the coming weeks.
Table 4: Drillhole assays through reported mineralised intercept (Au) of
drillhole CBRC0050
Hole ID From m To m Au (g/t)
CBRC0050 65 66 3.23
CBRC0050 66 67 4.92
CBRC0050 67 68 5.24
CBRC0050 68 69 0.58
CBRC0050 69 70 0.13
CBRC0050 70 71 0.24
CBRC0050 71 72 0.07
CBRC0050 72 73 0.14
CBRC0050 73 74 3.83
CBRC0050 74 75 0.84
CBRC0050 75 76 0.33
CBRC0050 76 77 0.25
CBRC0050 77 78 0.15
CBRC0050 78 79 0.25
CBRC0050 79 80 0.50
CBRC0050 80 81 0.25
CBRC0050 81 82 0.38
CBRC0050 82 83 0.12
CBRC0050 83 84 2.38
CBRC0050 84 85 1.27
CBRC0050 85 86 0.78
CBRC0050 86 87 0.41
CBRC0050 87 88 0.34
CBRC0050 88 89 0.15
CBRC0050 89 90 0.84
CBRC0050 90 91 0.61
CBRC0050 91 92 0.54
CBRC0050 92 93 0.55
CBRC0050 93 94 0.91
CBRC0050 94 95 0.19
CBRC0050 95 96 0.85
CBRC0050 96 97 0.92
CBRC0050 97 98 1.99
CBRC0050 98 99 0.36
CBRC0050 99 100 0.20
CBRC0050 100 101 0.08
CBRC0050 101 102 0.37
CBRC0050 102 103 0.29
CBRC0050 103 104 1.46
Appendix 1: JORC Code, 2012 Edition - Table 1
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
Criteria JORC Code explanation Commentary
Sampling techniques · Nature and quality of sampling (eg cut channels, random chips, or · Sampling during Cobra Resources' 2021 RC drilling programme at the
specific specialised industry standard measurement tools appropriate to the Clarke prospect was obtained through RC drilling methods.
minerals under investigation, such as downhole gamma sondes, or handheld XRF
instruments, etc). These examples should not be taken as limiting the broad · Historic RC and RAB drilling methods have been employed at Clarke and
meaning of sampling. Baggy Green prospects since 2000. Rotary air-core drilling occurred earlier in
2021 and was used to aid in the programme design but have not been used for
· Include reference to measures taken to ensure sample representivity grade estimations or defining results that are reported in this announcement.
and the appropriate calibration of any measurement tools or systems used.
· Samples were collected via a Metzke cone splitter mounted to the
· Aspects of the determination of mineralisation that are Material to cyclone. 1m samples were managed through chute and butterfly valve to produce
the Public Report. a 2-4 kg sample. Samples were taken from the point of collar, but only samples
from the commencement of saprolite were selected for analysis.
· In cases where 'industry standard' work has been done this would be
relatively simple (eg 'reverse circulation drilling was used to obtain 1 m · Samples submitted to the Genalysis Intertek Laboratories, Adelaide,
samples from which 3 kg was pulverised to produce a 30 g charge for fire and pulverised to produce the 50 g fire assay charge.
assay'). In other cases, more explanation may be required, such as where there
is coarse gold that has inherent sampling problems. Unusual commodities or
mineralisation types (eg submarine nodules) may warrant disclosure of detailed
information.
Drilling techniques · Drill type (eg core, reverse circulation, open-hole hammer, rotary · Drilling completed by Bullion Drilling Pty Ltd using 5 ¾" reverse
air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or circulation drilling techniques from a Schramm T685WS rig with an auxiliary
standard tube, depth of diamond tails, face-sampling bit or other type, compressor.
whether core is oriented and if so, by what method, etc).
· 2020 RC Drilling was undertaken by Hagstrom Drilling using an Austrex
AC/RC rig using a 140 mm bit.
Drill sample recovery · Method of recording and assessing core and chip sample recoveries and · Sample recovery was generally good with water being intersected in
results assessed. 10% of the drilled holes. All samples were recorded for sample type, quality
and contamination potential and entered within a sample log.
· Measures taken to maximise sample recovery and ensure representative
nature of the samples. · In general, sample recoveries were good with 35-50 kg for each one
metre interval being recovered.
· Whether a relationship exists between sample recovery and grade and
whether sample bias may have occurred due to preferential loss/gain of · No relationships between sample recovery and grade have been
fine/coarse material. identified.
Logging · Whether core and chip samples have been geologically and · All drill samples were logged by an experienced geologist at the time
geotechnically logged to a level of detail to support appropriate Mineral of drilling. Lithology, colour, weathering and moisture were documented.
Resource estimation, mining studies and metallurgical studies.
· All drilled metres were logged.
· Whether logging is qualitative or quantitative in nature. Core (or
costean, channel, etc) photography. · Logging is generally qualitative in nature.
· The total length and percentage of the relevant intersections logged. · All RC drill metres have been geologically logged (2,144m in total).
Sub-sampling techniques and sample preparation · If core, whether cut or sawn and whether quarter, half or all core · Sample recovery from hole CBRC0042 was considered excessive. All
taken. samples were split using a secondary riffle splitter to obtain a 50% sample
reduction to produce a more manageable sample. Once chute and valve settings
· If non-core, whether riffled, tube sampled, rotary split, etc and were adjusted to provide suitable sample returns, no further sub-sampling was
whether sampled wet or dry. required.
· For all sample types, the nature, quality and appropriateness of the · Additional sub-sampling was performed through the preparation and
sample preparation technique. processing of samples according to the laboratory's internal protocols.
· Quality control procedures adopted for all sub-sampling stages to · Duplicate samples were collected from the second chute on the cyclone
maximise representivity of samples. splitter at a 1 in 20 sample frequency.
· Measures taken to ensure that the sampling is representative of the · Sample sizes were appropriate for the material being sampled.
in situ material collected, including for instance results for field
duplicate/second-half sampling.
· Whether sample sizes are appropriate to the grain size of the
material being sampled.
Quality of assay data and laboratory tests · The nature, quality and appropriateness of the assaying and · Samples were submitted to Genalysis Intertek Laboratories, Adelaide,
laboratory procedures used and whether the technique is considered partial or for preparation and analysis.
total.
· Gold quantity was analysed using 50 g fire assay techniques
· For geophysical tools, spectrometers, handheld XRF instruments, etc, (FA50/OE04) that utilise a 50 g lead collection fire assay with ICP-OES finish
the parameters used in determining the analysis including instrument make and to deliver reportable precision to 0.005 ppm.
model, reading times, calibrations factors applied and their derivation, etc.
· Multi-element geochemistry was digested by four acid ICP-MS and
· Nature of quality control procedures adopted (eg standards, blanks, analysed for Ag, As, Bi, Ca, Cd, Ce, Co, Cr, Cs, Cu, Fe, Li, Mg, Mn, Mo, Ni,
duplicates, external laboratory checks) and whether acceptable levels of Pb, Pd, Pt, Sb, Se, S, Sn, Sr, Te, U, V, W, Y and Zn.
accuracy (ie lack of bias) and precision have been established.
· Saprolite zones of all holes drilled in 2021 were identified and
highlighted to analyse for lanthanide elements.
· 40 additional pulp samples were identified from CBRC0009 (drilled in
2020) to analyse for additional lanthanide elements by 4-acid ICP-MS and
analysed for Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu.
· Field blanks and standards were submitted at a frequency of 1 in 20
samples.
· Field duplicate samples were submitted at a frequency of 1 in 20
samples.
· Reported assays are to acceptable levels of accuracy and precision.
· Samples from the 2020 RC programme analysed by ALS, Adelaide, using
AU-GA22 50 g charge. Muti-elements (48) for all samples we analysed using
ME-MS61, a 4-acid digest method with an ICP-MS finish.
Verification of sampling and assaying · The verification of significant intersections by either independent · Sampling data was recorded in field books, checked upon digitising
or alternative company personnel. and transferred to database.
· The use of twinned holes. · Compositing of assays was undertaken and reviewed by Cobra staff.
· Documentation of primary data, data entry procedures, data · Original copies of lab assay data are retained digitally on the Cobra
verification, data storage (physical and electronic) protocols. server for future reference.
· Discuss any adjustment to assay data. · Physical copies of field sampling books and field geological logs are
retained by Cobra for future reference.
· Historic significant intercepts have been calculated using datamine
software with a 0.5 g/t cut-off and a maximum internal dilution of 3m.
· Significant intercepts have been prepared by Mr Rupert Verco and
reviewed by Mr Robert Blythman.
Location of data points · Accuracy and quality of surveys used to locate drill holes (collar · Collar locations were surveyed using Leica CS20 GNSS base and rover
and downhole surveys), trenches, mine workings and other locations used in with 0.05cm instrument precision.
Mineral Resource estimation.
· Locations are recorded in geodetic datum GDA 94 zone 53.
· Specification of the grid system used.
· Downhole surveys were undertaken by Bullion Drilling using a Reflex
· Quality and adequacy of topographic control. TN14 Gyro compass and were taken at 10m intervals at the completion of the
hole.
· Downhole survey azimuths have been converted from true north to
geodetic datum GDA 94 zone 53.
Data spacing and distribution · Data spacing for reporting of Exploration Results. · Hole CBRC0042 was drilled 75m North of CBRC0009 and was drilled to
the northeast.
· Whether the data spacing and distribution is sufficient to establish
the degree of geological and grade continuity appropriate for the Mineral · Transect CBRC0043 was collared 25m north and 50m east of CBRC0009 and
Resource and Ore Reserve estimation procedure(s) and classifications applied. drilled to the southwest. All other holes were drilled to the southeast on
northwest transects at a spacing of 50m by 100m.
· Whether sample compositing has been applied.
· Hole dips vary between 60 and 70 degrees.
· No sample compositing has been applied.
Orientation of data in relation to geological structure · Whether the orientation of sampling achieves unbiased sampling of · The programme was designed to test alternate interpretations on
possible structures and the extent to which this is known, considering the structural orientation.
deposit type.
· Holes CBRC0042 and CBRC0043 were scissored to test the orientation of
· If the relationship between the drilling orientation and the mineralisation. The results support a northwest strike and an apparent
orientation of key mineralised structures is considered to have introduced a northeast dip. Further results are required to confirm the continuity and
sampling bias, this should be assessed and reported if material. validity of the current interpretation.
· Gold results are not presented as true width but are not considered
to present any down-dip bias.
· Rare Earth intercepts have been presented as both downhole and true
width intercepts. The nature of mineralisation reflects the weathering profile
of the saprolite and is therefore horizontal in nature. Reported true widths
are calculated as vertical.
Sample security · The measures taken to ensure sample security. · Transportation of samples to Adelaide was undertaken by a competent
independent contractor. Samples were packaged in zip tied polyweave bags in
bundles of five samples and transported in larger bulka bags by batch while
being transported.
Audits or reviews · The results of any audits or reviews of sampling techniques and data. · No audit or review has been undertaken.
· Genalysis Intertek Laboratories Adelaide are a National Association
of Testing Authorities ("NATA") accredited laboratory, recognition of their
analytical competence.
Appendix 2: Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
Criteria JORC Code explanation Commentary
Mineral tenement and land tenure status · Type, reference name/number, location and ownership including · This drilling programme has been carried out on EL 6131, currently
agreements or material issues with third parties such as joint ventures, owned 100% by Peninsula Resources limited, a wholly owned subsidiary of
partnerships, overriding royalties, native title interests, historical sites, Andromeda Metals Limited.
wilderness or national park and environmental settings.
· Newcrest Mining Limited retains a 1.5% NSR royalty over future
· The security of the tenure held at the time of reporting along with mineral production from both exploration licences.
any known impediments to obtaining a licence to operate in the area.
· Baggy Green, Clarke, Laker and the IOCG targets are located within
Pinkawillinie Conservation Park. Native Title Agreement has been negotiated
with the NT Claimant and has been registered with the SA Government.
· Aboriginal heritage surveys have been completed over the Baggy Green
project area, with no sites located in the immediate vicinity.
· A Native Title Agreement is in place with the relevant Native Title
party.
Exploration done by other parties · Acknowledgment and appraisal of exploration by other parties. · On-ground exploration completed prior to Andromeda Metals' work was
limited to 400m spaced soil geochemistry completed by Newcrest Mining Limited
over the Barns prospect.
· Other than the flying of regional airborne geophysics and coarse
spaced ground gravity, there has been no recorded exploration in the vicinity
of the Baggy Green deposit prior to Andromeda Metals' work.
Geology · Deposit type, geological setting and style of mineralisation. · The deposits are considered to be either lode gold or intrusion type
mineralisation related to the 1590 Ma Hiltaba/GRV tectonothermal event.
· Gold mineralisation has a spatial association with mafic
intrusions/granodiorite alteration and is associated with metasomatic
alteration of host rocks.
· Rare earth minerals occur within the kaolinised saprolite horizon.
Preliminary XRD analyses performed by the CSIRO supports IAC mineralisation.
Florencite and monazite were also detected. Further work is planned to
define mineralogy and nature of mineral occurrence.
· A summary of all information material to the understanding of the · The report includes a tabulation of drillhole collar information and
exploration results including a tabulation of the following information for associated interval grades to allow an understanding of the results reported
all material drill holes: herein.
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, · Reported summary intercepts are weighted averages based on length.
maximum and/or minimum grade truncations (eg cutting of high grades) and
cut-off grades are usually material and should be stated. · Rare earth intercepts have been presented as both down hole and true
width intercepts. The nature of mineralisation reflects the weathering profile
· Where aggregate intercepts incorporate short lengths of high-grade of the saprolite and is therefore horizontal in nature. Average intercept
results and longer lengths of low-grade results, the procedure used for such widths and grade have been reported using datamines true width calculator to
aggregation should be stated and some typical examples of such aggregations account for downhole surveys.
should be shown in detail.
· Rare earth results are reported with a 300 ppm TREO cut-over grade
· The assumptions used for any reporting of metal equivalent values and a maximum internal dilution of 5m.
should be clearly stated.
· Assayed intervals through reported intercepts are tabulated in the
body of this report.
· No metal equivalent values have been calculated.
· REE analysis was originally reported in elemental form and has been
converted to relevant oxide concentrations in line with industry standards.
Conversion factors tabulated below:
Element Oxide Factor
Cerium CeO2 1.2284
Dysprosium Dy2O3 1.1477
Erbium Er2O3 1.1435
Europium Eu2O3 1.1579
Gadolinium Gd2O3 1.1526
Holmium Ho2O3 1.1455
Lanthanum La2O3 1.1728
Lutetium Lu2O3 1.1371
Neodymium Nd2O3 1.1664
Praseodymium Pr2O3 1.1703
Scandium Sc2O3 1.5338
Samarium Sm2O3 1.1596
Terbium Tb2O3 1.151
Thulium Tm2O3 1.1421
Yttrium Y2O3 1.2699
Ytterbium Yb2O3 1.1387
· The reporting of REE oxides is done so in accordance with industry
standards with the following calculations applied:
§ TREO = La2O3 + CeO2 + Pr6O11 + Nd2O3 + Sm2O3 + Eu2O3 + Gd2O3 + Tb4O7 +
Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 + Yb2O3 + Lu2O3 + Y2O3
§ CREO = Nd2O3 + Eu2O3 + Tb4O7 + Dy2O3 + Y2O3
§ LREO = La2O3 + CeO2 + Pr6O11 + Nd2O3
§ HREO = Sm2O3 + Eu2O3 + Gd2O3 + Tb4O7 + Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 +
Yb2O3 + Lu2O3 + Y2O3
§ NdPr = Nd2O3 + Pr6O11
§ TREO-Ce = TREO - CeO2
§ % Nd = Nd2O3/ TREO
§ %Pr = Pr6O11/TREO
§ %Dy = Dy2O3/TREO
§ %HREO = HREO/TREO
§ %LREO = LREO/TREO
Relationship between mineralisation widths and intercept lengths · These relationships are particularly important in the reporting of · This drilling programme is designed to confirm the orientation and
Exploration Results. continuity of mineralisation. Preliminary results support unbiased testing of
mineralized structures.
· If the geometry of the mineralisation with respect to the drill hole
angle is known, its nature should be reported. · Previous holes drilled have been drilled in several orientations due
to the unknown nature of mineralisation.
· If it is not known and only the downhole lengths are reported, there
should be a clear statement to this effect (eg 'downhole length, true width · The work completed to date is not considered robust to adequately
not known'). define mineralisation geometry.
Diagrams · Appropriate maps and sections (with scales) and tabulations of · Plan and section maps are referenced that demonstrate results of
intercepts should be included for any significant discovery being reported. interest.
These should include, but not be limited to, a plan view of drill hole collar
locations and appropriate sectional views.
Balanced reporting · Where comprehensive reporting of all Exploration Results is not · Referenced plans detail the extent of drilling and the locations of
practicable, representative reporting of both low and high grades and/or both high and low grades. Comprehensive results are reported.
widths should be practiced to avoid misleading reporting of Exploration
Results.
Other substantive exploration data · Other exploration data, if meaningful and material, should be · Significant intercepts of reported previous drilling is tabulated
reported including (but not limited to): geological observations; geophysical (CBRC0009). Historic significant intercepts from Clarke as tabulated in
survey results; geochemical survey results; bulk samples - size and method of appendix 3.
treatment; metallurgical test results; bulk density, groundwater, geotechnical
and rock characteristics; potential deleterious or contaminating substances.
Further work · The nature and scale of planned further work (eg tests for lateral · Further RC drilling is planned to test for both lateral and depth
extensions or depth extensions or large-scale step-out drilling). extensions. The complete results from this programme will form the foundation
for a maiden resource estimation at Clarke.
· Diagrams clearly highlighting the areas of possible extensions,
including the main geological interpretations and future drilling areas,
provided this information is not commercially sensitive.
· The reporting of REE oxides is done so in accordance with industry
standards with the following calculations applied:
§ TREO = La2O3 + CeO2 + Pr6O11 + Nd2O3 + Sm2O3 + Eu2O3 + Gd2O3 + Tb4O7 +
Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 + Yb2O3 + Lu2O3 + Y2O3
§ CREO = Nd2O3 + Eu2O3 + Tb4O7 + Dy2O3 + Y2O3
§ LREO = La2O3 + CeO2 + Pr6O11 + Nd2O3
§ HREO = Sm2O3 + Eu2O3 + Gd2O3 + Tb4O7 + Dy2O3 + Ho2O3 + Er2O3 + Tm2O3 +
Yb2O3 + Lu2O3 + Y2O3
§ NdPr = Nd2O3 + Pr6O11
§ TREO-Ce = TREO - CeO2
§ % Nd = Nd2O3/ TREO
§ %Pr = Pr6O11/TREO
§ %Dy = Dy2O3/TREO
§ %HREO = HREO/TREO
§ %LREO = LREO/TREO
Relationship between mineralisation widths and intercept lengths
· These relationships are particularly important in the reporting of
Exploration Results.
· If the geometry of the mineralisation with respect to the drill hole
angle is known, its nature should be reported.
· If it is not known and only the downhole lengths are reported, there
should be a clear statement to this effect (eg 'downhole length, true width
not known').
· This drilling programme is designed to confirm the orientation and
continuity of mineralisation. Preliminary results support unbiased testing of
mineralized structures.
· Previous holes drilled have been drilled in several orientations due
to the unknown nature of mineralisation.
· The work completed to date is not considered robust to adequately
define mineralisation geometry.
Diagrams
· Appropriate maps and sections (with scales) and tabulations of
intercepts should be included for any significant discovery being reported.
These should include, but not be limited to, a plan view of drill hole collar
locations and appropriate sectional views.
· Plan and section maps are referenced that demonstrate results of
interest.
Balanced reporting
· Where comprehensive reporting of all Exploration Results is not
practicable, representative reporting of both low and high grades and/or
widths should be practiced to avoid misleading reporting of Exploration
Results.
· Referenced plans detail the extent of drilling and the locations of
both high and low grades. Comprehensive results are reported.
Other substantive exploration data
· Other exploration data, if meaningful and material, should be
reported including (but not limited to): geological observations; geophysical
survey results; geochemical survey results; bulk samples - size and method of
treatment; metallurgical test results; bulk density, groundwater, geotechnical
and rock characteristics; potential deleterious or contaminating substances.
· Significant intercepts of reported previous drilling is tabulated
(CBRC0009). Historic significant intercepts from Clarke as tabulated in
appendix 3.
Further work
· The nature and scale of planned further work (eg tests for lateral
extensions or depth extensions or large-scale step-out drilling).
· Diagrams clearly highlighting the areas of possible extensions,
including the main geological interpretations and future drilling areas,
provided this information is not commercially sensitive.
· Further RC drilling is planned to test for both lateral and depth
extensions. The complete results from this programme will form the foundation
for a maiden resource estimation at Clarke.
Appendix 3: Drillhole data - 1m samples through reported intercepts.
Table 5: Reporting through rare earth intercepts
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0044 33 34 291 5.6 3.1 1.5 6.7 1.1 67.2 0.4 53 15.1 8.7 1.0 0.4 29.3 2.9 487 196 435 52 10.7% 14.0% 1.1% 30.5 6.5
CBRC0044 34 35 353 8.7 4.4 2.3 10.8 1.6 99.7 0.5 84 22.9 13.9 1.6 0.6 44.0 4.1 652 299 573 79 12.1% 16.4% 1.3% 32.6 7.7
CBRC0044 35 36 503 20.8 10.6 5.8 26.8 3.8 237.2 1.1 211 55.6 34.6 3.8 1.4 102.7 8.6 1,227 724 1,042 185 15.1% 21.7% 1.7% 32.8 12.9
CBRC0044 36 37 704 14.9 7.9 4.0 18.2 2.8 151.7 0.9 138 38.4 23.8 2.7 1.1 70.3 7.2 1,186 482 1,056 130 11.0% 14.9% 1.3% 31.7 10.2
CBRC0044 37 38 213 12.6 6.7 4.0 16.5 2.3 146.6 0.9 155 45.4 25.9 2.4 1.0 50.7 6.5 690 477 587 104 15.0% 29.1% 1.8% 27.1 7.1
CBRC0044 38 39 242 17.6 9.9 4.9 21.9 3.4 176.8 1.3 173 47.8 29.0 3.1 1.4 85.8 9.3 827 585 668 159 19.2% 26.7% 2.1% 27.6 6.3
CBRC0044 39 40 135 14.3 7.5 4.3 18.9 2.6 160.2 1.0 151 42.8 25.2 2.6 1.1 64.9 7.1 639 504 515 124 19.5% 30.4% 2.2% 23.7 4.0
CBRC0044 40 41 209 18.4 8.1 5.8 24.5 3.1 225.2 0.9 198 56.7 34.5 3.4 1.1 76.1 6.9 872 663 724 148 17.0% 29.2% 2.1% 26.9 3.9
CBRC0044 41 42 131 15.3 7.7 4.9 21.3 2.8 181.6 1.0 169 47.4 29.0 2.9 1.1 69.2 6.9 691 560 558 133 19.3% 31.3% 2.2% 27.8 4.5
CBRC0044 42 43 132 19.5 9.2 5.8 26.5 3.4 196.0 1.1 181 49.8 33.2 3.7 1.3 83.1 8.2 753 621 591 162 21.5% 30.6% 2.6% 29.1 4.2
CBRC0044 43 44 192 39.3 20.0 10.0 48.7 7.3 336.9 2.4 272 74.1 51.0 7.0 2.8 201.1 17.4 1,281 1,090 925 356 27.8% 27.0% 3.1% 22.8 4.8
CBRC0044 44 45 358 72.9 41.6 15.4 81.2 14.3 483.2 5.0 376 100.0 71.1 12.5 5.7 461.6 35.1 2,133 1,775 1,388 745 34.9% 22.3% 3.4% 18.8 5.1
CBRC0044 45 46 160 10.6 6.2 2.3 11.6 2.1 88.4 0.8 68 19.2 12.5 1.7 0.9 66.2 5.4 456 296 348 108 23.6% 19.1% 2.3% 21.4 2.9
CBRC0044 46 47 158 10.8 6.0 2.5 11.8 2.1 90.4 0.8 71 19.4 13.0 1.9 0.9 58.9 5.5 452 295 351 101 22.3% 19.9% 2.4% 17.8 3.2
CBRC0044 47 48 133 7.9 5.0 1.7 8.1 1.6 61.6 0.7 47 13.1 8.7 1.3 0.7 48.3 4.9 344 211 264 80 23.3% 17.6% 2.3% 20.1 4.3
CBRC0044 48 49 145 7.0 3.8 1.7 7.9 1.3 60.9 0.5 51 14.2 9.3 1.2 0.5 38.1 3.5 346 201 281 66 18.9% 18.8% 2.0% 22.7 4.2
CBRC0044 49 50 144 5.3 3.0 1.4 6.2 1.0 50.7 0.4 45 12.6 7.7 0.9 0.4 28.9 3.0 311 167 260 51 16.3% 18.6% 1.7% 21.2 4.3
CBRC0044 50 51 123 5.0 3.1 1.2 5.5 1.0 42.7 0.4 38 10.2 6.3 0.8 0.4 29.3 3.1 270 147 220 50 18.5% 17.7% 1.9% 25.1 4.6
CBRC0044 51 52 207 14.3 6.9 3.3 16.3 2.7 94.7 0.8 83 20.8 16.5 2.5 1.0 71.2 6.0 547 340 422 125 22.8% 19.0% 2.6% 25.5 5.0
CBRC0044 52 53 139 15.6 8.6 3.4 16.5 3.0 73.1 1.1 80 18.9 16.2 2.6 1.2 87.1 7.8 474 335 327 147 31.0% 20.8% 3.3% 14.1 4.8
CBRC0044 53 54 157 9.5 5.4 2.2 10.9 1.9 83.7 0.7 68 18.6 12.1 1.6 0.8 50.0 5.3 428 271 340 88 20.6% 20.3% 2.2% 24.4 5.0
CBRC0043 41 42 327 26.6 13.3 8.6 33.4 4.5 197.9 1.6 244 67.2 46.3 4.8 1.9 107.3 12.8 1,097 770 882 215 19.6% 28.3% 2.4% 25.9 6.2
CBRC0043 42 43 398 66.4 34.8 19.2 85.7 12.0 543.9 4.5 534 145.8 97.3 12.1 5.0 309.7 33.7 2,303 1,904 1,720 583 25.3% 29.5% 2.9% 25.9 5.7
CBRC0043 43 44 275 27.1 14.7 7.5 33.0 4.9 211.6 1.8 198 54.5 36.7 4.8 2.1 127.1 13.2 1,012 737 776 236 23.3% 25.0% 2.7% 26.6 5.1
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0043 44 45 238 20.3 11.5 5.2 23.4 3.7 154.4 1.4 134 36.8 24.8 3.4 1.6 105.0 10.4 774 536 588 186 24.0% 22.1% 2.6% 25.7 5.1
CBRC0043 45 46 172 12.9 7.8 3.0 14.3 2.5 87.4 1.0 74 20.3 14.3 2.2 1.1 81.2 6.9 501 329 368 133 26.5% 18.8% 2.6% 23.6 5.5
CBRC0043 46 47 189 14.2 9.1 3.1 14.6 2.8 83.1 1.2 71 19.5 14.5 2.3 1.3 95.9 8.4 531 341 378 153 28.8% 17.1% 2.7% 26.6 6.6
CBRC0043 47 48 173 10.4 5.9 2.6 11.4 1.9 79.2 0.7 68 18.8 12.7 1.7 0.8 59.4 5.0 451 278 352 100 22.1% 19.2% 2.3% 22.3 5.6
CBRC0043 48 49 204 12.0 6.8 3.1 12.8 2.3 88.9 0.8 78 21.8 14.9 2.0 0.9 70.7 5.9 524 321 407 117 22.4% 19.0% 2.3% 25.6 4.9
CBRC0043 49 50 155 8.8 4.7 2.2 9.5 1.6 67.6 0.5 59 16.1 11.2 1.5 0.6 48.9 4.1 392 237 310 83 21.0% 19.2% 2.3% 17.4 4.0
CBRC0043 50 51 112 7.2 4.1 1.9 7.7 1.3 51.0 0.5 46 12.4 8.9 1.2 0.5 38.9 3.5 298 185 231 67 22.5% 19.7% 2.4% 11.8 3.5
CBRC0043 51 52 254 11.6 5.6 3.3 13.4 2.0 110.8 0.5 94 26.8 16.7 2.0 0.7 55.1 4.4 602 347 503 99 16.4% 20.1% 1.9% 23.3 4.0
CBRC0043 52 53 234 10.7 5.3 3.1 12.4 1.8 103.0 0.6 88 24.1 15.3 1.9 0.7 52.7 4.5 559 324 465 94 16.8% 20.1% 1.9% 19.5 4.7
CBRC0043 53 54 224 10.5 5.2 3.1 12.2 1.8 96.4 0.5 82 23.6 14.8 1.9 0.7 53.4 4.3 534 310 440 94 17.5% 19.8% 2.0% 18.6 5.0
CBRC0043 54 55 229 11.5 5.6 3.2 12.9 1.9 100.8 0.6 88 24.6 16.2 2.1 0.7 54.9 4.6 557 328 459 98 17.6% 20.3% 2.1% 19.0 3.9
CBRC0045 33 34 697 14.3 7.7 3.5 16.3 2.8 101.4 0.8 93 24.9 18.4 2.5 1.0 72.4 6.3 1,062 365 935 128 12.0% 11.1% 1.3% 41.4 9.5
CBRC0045 34 35 539 20.5 10.5 5.0 24.0 3.8 170.2 1.1 150 40.2 28.7 3.6 1.4 99.1 8.9 1,106 567 929 178 16.1% 17.2% 1.8% 35.9 8.7
CBRC0045 35 36 347 14.2 7.9 3.6 17.5 2.8 141.8 1.0 130 35.3 22.5 2.5 1.1 76.8 7.1 811 464 677 134 16.6% 20.4% 1.8% 36.4 8.0
CBRC0045 36 37 219 10.0 5.6 2.5 12.0 2.0 92.9 0.7 82 22.4 14.8 1.7 0.8 57.9 5.3 530 311 431 99 18.6% 19.7% 1.9% 29.2 6.6
CBRC0045 37 38 173 6.3 4.0 1.4 6.8 1.3 43.5 0.6 40 11.1 8.1 1.1 0.6 39.1 4.0 341 168 276 65 19.1% 15.1% 1.8% 24.4 7.1
CBRC0045 38 39 159 4.3 2.9 0.8 4.1 0.9 28.9 0.5 23 6.4 4.8 0.7 0.4 27.4 3.1 268 109 223 45 16.9% 11.2% 1.6% 19.8 4.5
CBRC0045 39 40 769 51.5 23.2 15.0 66.7 9.0 457.5 2.1 450 121.7 86.8 10.1 3.1 226.0 18.8 2,312 1,542 1,886 426 18.4% 24.8% 2.2% 25.5 7.8
CBRC0045 40 41 355 50.4 23.9 12.6 58.6 8.9 374.3 2.7 350 93.3 67.8 9.2 3.4 200.1 22.0 1,631 1,277 1,240 392 24.0% 27.2% 3.1% 29.8 5.2
CBRC0045 41 42 155 8.1 4.3 1.9 10.0 1.5 64.2 0.5 60 15.7 11.5 1.5 0.6 40.7 4.0 380 225 307 73 19.3% 20.0% 2.1% 21.3 3.6
CBRC0045 42 43 113 4.6 2.6 1.2 5.7 0.9 44.0 0.3 35 9.5 6.3 0.8 0.4 24.3 2.6 252 138 208 44 17.3% 17.7% 1.8% 18.9 2.8
CBRC0045 43 44 75 2.5 1.6 0.7 2.9 0.5 20.9 0.2 19 5.2 3.4 0.4 0.2 14.7 1.7 149 74 123 26 17.1% 16.2% 1.7% 16.0 2.1
CBRC0045 44 45 126 6.6 3.6 1.7 8.2 1.3 57.0 0.4 48 12.3 9.1 1.2 0.5 35.7 3.2 314 188 252 62 19.9% 19.1% 2.1% 22.8 2.5
CBRC0045 45 46 90 6.4 4.3 1.4 7.0 1.4 38.1 0.6 34 9.1 7.0 1.1 0.7 43.8 4.3 249 160 178 71 28.5% 17.4% 2.6% 20.3 3.5
CBRC0045 46 47 203 18.6 10.4 4.6 21.8 3.6 133.6 1.3 119 32.3 23.6 3.3 1.4 100.7 9.3 687 484 512 175 25.5% 22.1% 2.7% 26.2 4.9
CBRC0045 47 48 139 8.8 5.2 2.0 10.2 1.8 68.4 0.8 58 15.8 11.1 1.5 0.7 49.5 5.0 378 239 292 86 22.6% 19.6% 2.3% 24.7 3.7
CBRC0045 48 49 127 8.0 5.1 1.7 8.8 1.7 58.1 0.8 50 13.2 9.4 1.4 0.8 51.4 5.0 342 215 258 85 24.7% 18.4% 2.3% 20.8 3.8
CBRC0045 49 50 105 6.9 4.8 1.5 7.5 1.5 52.1 0.8 44 12.1 8.4 1.1 0.7 50.0 5.0 301 196 221 80 26.5% 18.5% 2.3% 18.9 3.4
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0045 50 51 125 6.3 4.1 1.5 7.2 1.4 52.8 0.6 45 12.2 8.2 1.2 0.6 39.7 4.1 310 184 243 67 21.5% 18.3% 2.0% 20.0 4.3
CBRC0045 51 52 91 4.5 2.9 1.3 5.4 0.9 40.4 0.4 35 9.7 6.3 0.8 0.4 27.8 2.8 230 139 183 47 20.6% 19.4% 2.0% 19.2 3.6
CBRC0045 52 53 92 5.2 3.2 1.4 6.0 1.1 42.2 0.5 38 10.3 7.2 0.9 0.4 30.2 3.1 243 150 190 52 21.5% 20.0% 2.1% 19.0 3.7
CBRC0045 53 54 78 8.1 5.1 1.9 8.7 1.7 45.9 0.8 41 10.5 8.5 1.3 0.7 48.0 4.9 265 187 184 81 30.7% 19.4% 3.1% 21.7 4.7
CBRC0045 54 55 388 59.5 40.2 9.4 55.9 13.2 184.5 5.4 190 45.6 43.9 9.3 5.6 438.1 36.9 1,526 1,137 852 674 44.1% 15.4% 3.9% 20.4 6.2
CBRC0045 55 56 126 25.2 20.9 3.7 21.6 6.4 56.0 3.1 61 13.7 15.1 3.7 3.0 250.5 19.8 629 503 271 358 56.8% 11.9% 4.0% 10.3 3.6
CBRC0045 56 57 150 44.5 37.4 6.3 38.8 11.3 68.7 5.4 92 18.1 24.2 6.4 5.3 459.7 35.7 1,004 854 353 651 64.8% 11.0% 4.4% 9.0 3.2
CBRC0046 21 22 385 11.8 5.3 3.7 16.4 2.0 143.9 0.6 141 39.4 23.2 2.2 0.7 50.7 4.0 829 445 732 97 11.7% 21.7% 1.4% 56.5 8.7
CBRC0046 22 23 307 13.8 6.4 4.4 19.0 2.3 175.1 0.7 173 48.9 28.2 2.6 0.8 62.6 4.7 849 542 732 117 13.8% 26.1% 1.6% 47.2 9.6
CBRC0046 23 24 364 17.1 8.3 5.1 23.0 3.0 217.6 0.9 197 55.4 32.5 3.2 1.1 80.6 6.3 1,015 651 866 149 14.6% 24.8% 1.7% 43.4 6.7
CBRC0046 24 25 280 15.6 8.1 4.3 19.5 2.8 183.7 0.9 159 45.0 26.5 2.8 1.0 80.8 6.3 836 556 694 142 17.0% 24.4% 1.9% 31.9 5.2
CBRC0046 25 26 290 19.6 10.0 5.8 25.2 3.5 211.7 1.1 206 57.5 35.1 3.5 1.3 100.2 8.0 979 689 801 178 18.2% 27.0% 2.0% 36.4 5.3
CBRC0046 26 27 213 14.1 7.7 4.0 18.0 2.6 159.1 0.9 140 39.7 24.5 2.5 1.0 80.2 5.8 713 500 576 137 19.2% 25.3% 2.0% 27.6 3.2
CBRC0046 27 28 361 17.9 8.9 5.4 24.3 3.2 218.1 1.0 196 54.7 32.8 3.3 1.1 91.2 6.9 1,025 665 862 163 15.9% 24.4% 1.7% 36.1 6.6
CBRC0046 28 29 304 19.9 11.0 5.4 24.4 3.6 204.4 1.3 183 50.5 31.3 3.5 1.4 115.1 8.6 967 663 773 194 20.1% 24.1% 2.1% 33.0 3.9
CBRC0046 29 30 369 24.7 13.3 6.4 31.3 4.5 223.2 1.5 214 58.3 37.3 4.4 1.7 139.9 10.0 1,140 771 902 238 20.8% 23.9% 2.2% 40.7 3.8
CBRC0046 30 31 239 13.4 6.9 3.7 16.7 2.4 148.6 0.8 129 36.0 22.2 2.4 0.9 71.1 5.4 698 459 574 124 17.7% 23.6% 1.9% 32.5 4.7
CBRC0046 31 32 265 13.7 6.9 3.8 17.4 2.4 174.1 0.9 134 38.0 22.1 2.4 0.9 74.0 5.5 761 496 633 128 16.8% 22.6% 1.8% 32.3 3.4
CBRC0046 32 33 260 14.5 6.7 4.6 19.7 2.5 178.2 0.6 143 40.2 24.7 2.8 0.8 67.4 4.6 770 510 646 124 16.1% 23.7% 1.9% 22.8 2.9
CBRC0046 33 34 268 17.7 8.2 4.9 23.0 3.0 175.0 0.8 147 39.9 25.3 3.2 1.0 95.8 5.4 819 551 656 163 19.9% 22.9% 2.2% 19.3 3.6
CBRC0046 34 35 200 13.0 6.2 3.5 16.2 2.3 136.7 0.7 108 30.5 19.2 2.4 0.8 67.5 4.6 612 412 494 117 19.1% 22.7% 2.1% 28.5 2.5
CBRC0046 35 36 242 17.2 8.8 4.2 20.5 3.0 175.6 1.0 128 36.0 22.1 3.1 1.1 90.7 6.4 759 518 603 156 20.5% 21.6% 2.3% 30.4 2.7
CBRC0046 36 37 108 10.9 7.1 2.2 11.6 2.2 68.2 1.0 59 15.2 10.9 1.7 0.9 74.2 5.7 378 270 260 117 31.1% 19.5% 2.9% 23.4 2.4
CBRC0046 37 38 39 7.8 5.6 1.2 6.5 1.7 35.5 0.8 25 6.8 5.1 1.1 0.8 56.2 5.0 198 159 111 87 43.8% 16.1% 4.0% 19.3 2.5
CBRC0046 38 39 177 13.9 7.3 3.2 15.8 2.4 137.8 0.9 95 27.1 16.9 2.3 0.9 72.6 5.5 579 402 454 125 21.5% 21.1% 2.4% 37.9 3.3
CBRC0046 39 40 116 9.6 5.6 2.0 10.3 1.8 79.9 0.7 60 17.2 10.6 1.6 0.7 56.9 4.4 377 261 283 94 24.8% 20.4% 2.5% 29.7 2.8
CBRC0046 40 41 108 9.5 6.2 1.8 9.8 2.0 58.0 0.8 55 14.9 10.0 1.5 0.8 63.7 4.9 347 239 246 101 29.1% 20.0% 2.7% 32.3 2.8
CBRC0046 41 42 142 8.8 5.3 1.9 10.4 1.8 83.0 0.7 64 18.2 11.1 1.5 0.7 57.3 4.1 411 269 318 93 22.5% 20.0% 2.1% 35.4 2.7
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0046 42 43 79 6.5 3.8 1.5 7.3 1.3 62.5 0.5 43 12.6 7.6 1.1 0.5 39.1 3.1 270 190 205 65 24.0% 20.6% 2.4% 36.3 3.2
CBRC0046 43 44 266 13.2 6.6 3.9 17.7 2.4 127.7 0.7 121 33.0 21.0 2.4 0.8 70.9 4.7 693 426 569 123 17.8% 22.3% 1.9% 26.3 3.1
CBRC0046 44 45 323 15.3 8.8 3.8 19.3 3.0 136.8 1.1 133 35.8 23.2 2.7 1.2 93.7 6.9 808 484 652 156 19.3% 20.9% 1.9% 31.1 2.6
CBRC0046 45 46 126 6.1 4.0 1.4 7.1 1.2 54.2 0.6 50 13.7 8.5 1.0 0.6 38.4 3.6 316 190 252 64 20.2% 20.1% 1.9% 28.9 2.9
CBRC0046 46 47 254 6.1 3.5 1.7 9.0 1.1 106.4 0.5 89 26.2 13.6 1.1 0.5 36.4 3.3 553 299 489 63 11.4% 20.9% 1.1% 44.0 2.8
CBRC0046 47 48 140 5.4 3.0 1.4 7.0 1.0 67.1 0.4 56 15.8 9.3 1.0 0.4 30.9 2.7 341 202 288 53 15.5% 21.1% 1.6% 23.4 2.4
CBRC0046 48 49 164 8.1 5.2 1.7 9.8 1.6 72.0 0.8 62 17.0 10.5 1.3 0.7 53.2 4.4 412 248 325 87 21.1% 19.1% 2.0% 23.3 2.8
CBRC0046 49 50 108 4.4 2.7 1.2 5.6 0.8 53.4 0.4 42 12.0 7.2 0.8 0.4 25.3 2.5 267 158 223 44 16.5% 20.2% 1.6% 22.0 2.1
CBRC0046 50 51 174 6.5 3.9 1.6 8.3 1.2 77.9 0.6 66 18.8 10.9 1.1 0.5 36.6 3.6 412 238 348 64 15.5% 20.6% 1.6% 26.8 2.7
CBRC0046 51 52 384 15.4 8.8 3.9 20.1 2.9 178.1 1.2 150 40.7 24.6 2.7 1.2 91.1 7.1 931 547 777 154 16.6% 20.4% 1.7% 34.7 3.1
CBRC0046 52 53 337 31.2 20.3 7.0 32.6 6.4 172.3 2.4 166 42.4 30.3 4.9 2.6 254.9 15.0 1,125 788 748 377 33.5% 18.5% 2.8% 22.0 3.8
CBRC0046 53 54 350 39.6 29.1 6.7 42.9 9.0 228.4 4.1 171 39.7 30.1 6.0 3.9 365.2 24.4 1,350 1,000 819 531 39.3% 15.6% 2.9% 13.4 2.7
CBRC0046 54 55 339 16.3 11.2 3.6 20.2 3.5 170.9 1.5 133 36.5 20.7 2.7 1.5 144.3 8.7 913 574 700 213 23.4% 18.5% 1.8% 44.2 3.6
CBRC0046 55 56 250 14.9 9.3 4.3 17.8 2.9 123.0 1.2 114 30.6 19.5 2.5 1.2 110.9 7.5 710 460 538 173 24.3% 20.4% 2.1% 23.2 3.0
CBRC0046 56 57 145 6.5 3.9 1.8 8.0 1.3 58.4 0.5 55 14.9 9.3 1.1 0.5 45.0 3.2 355 210 283 72 20.3% 19.8% 1.8% 15.9 1.6
CBRC0046 57 58 263 9.1 5.0 2.2 12.4 1.7 127.6 0.6 100 28.6 15.7 1.6 0.6 57.9 3.9 631 368 535 95 15.1% 20.5% 1.4% 33.8 2.7
CBRC0046 58 59 427 12.5 7.1 3.0 17.5 2.3 200.7 1.0 149 43.3 23.5 2.3 0.9 75.6 5.7 972 545 844 128 13.2% 19.8% 1.3% 52.4 3.6
CBRC0046 59 60 281 9.1 5.1 2.0 12.1 1.7 126.4 0.7 101 28.6 15.8 1.6 0.7 54.5 4.3 645 364 553 92 14.2% 20.2% 1.4% 42.1 2.9
CBRC0046 60 61 291 9.4 5.5 2.2 12.7 1.8 130.7 0.8 104 29.9 16.5 1.6 0.7 57.7 4.8 670 379 572 97 14.5% 20.1% 1.4% 44.6 3.1
CBRC0046 61 62 199 7.0 3.9 1.8 9.6 1.3 88.3 0.5 73 20.7 12.1 1.3 0.5 41.6 3.1 464 265 393 71 15.2% 20.2% 1.5% 25.8 2.1
CBRC0046 62 63 201 7.3 4.0 1.7 9.6 1.4 94.6 0.6 76 21.2 12.2 1.3 0.5 42.9 3.4 478 276 405 73 15.2% 20.3% 1.5% 28.5 2.4
CBRC0046 63 64 153 6.6 3.9 1.6 8.7 1.2 70.5 0.5 58 16.0 9.7 1.1 0.5 42.8 3.1 378 225 308 70 18.5% 19.7% 1.8% 20.6 2.1
CBRC0047 20 21 246 6.7 3.2 2.4 8.8 1.2 82.5 0.4 75 22.0 12.9 1.2 0.4 27.8 2.9 493 247 438 55 11.2% 19.6% 1.4% 27.4 6.5
CBRC0047 21 22 128 6.7 3.5 2.5 9.0 1.2 82.2 0.5 84 24.3 14.6 1.2 0.5 29.4 3.3 391 263 333 58 14.8% 27.6% 1.7% 27.5 7.0
CBRC0047 22 23 186 9.5 5.0 3.4 12.3 1.7 110.4 0.7 112 33.0 19.5 1.8 0.7 42.4 4.7 543 357 461 82 15.1% 26.8% 1.7% 32.6 7.4
CBRC0047 23 24 69 5.7 3.3 1.8 7.0 1.1 55.8 0.5 56 16.3 10.2 1.0 0.5 28.3 3.3 260 190 208 52 20.1% 27.7% 2.2% 13.8 3.7
CBRC0047 24 25 113 10.2 5.9 2.9 11.8 1.9 120.6 0.8 80 23.0 14.6 1.8 0.8 56.0 5.5 449 336 352 98 21.7% 23.0% 2.3% 12.9 3.3
CBRC0047 25 26 240 43.9 27.7 11.6 52.6 9.3 348.8 3.4 304 83.3 55.5 7.6 3.8 334.5 23.2 1,549 1,309 1,032 518 33.4% 25.0% 2.8% 27.5 6.1
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0047 26 27 324 34.0 18.4 8.8 38.7 6.4 273.3 2.1 235 65.2 44.0 5.8 2.4 199.4 15.3 1,273 949 941 331 26.0% 23.6% 2.7% 21.7 10.0
CBRC0047 27 28 250 32.0 18.6 8.1 34.6 6.4 280.4 2.3 199 56.3 37.2 5.4 2.5 195.5 16.7 1,145 895 823 322 28.1% 22.3% 2.8% 31.1 9.1
CBRC0047 28 29 107 11.4 6.9 2.7 11.7 2.3 73.8 0.9 69 18.3 13.1 1.9 1.0 71.4 6.1 397 290 281 116 29.3% 21.9% 2.9% 23.9 5.6
CBRC0047 29 30 92 9.3 5.9 2.1 9.3 1.9 55.5 0.9 55 15.1 10.1 1.5 0.8 59.1 5.5 323 232 227 96 29.8% 21.6% 2.9% 23.9 4.2
CBRC0048 20 21 466 277.0 121.3 80.9 350.5 46.3 3100.8 13.1 2293 687.6 440.4 52.1 16.5 973.8 104.9 9,024 8,558 6,988 2037 22.6% 33.0% 3.1% 46.1 72.6
CBRC0048 21 22 120 14.2 8.1 3.6 16.4 2.7 172.4 1.0 107 33.3 19.4 2.5 1.1 73.2 7.3 583 462 453 130 22.3% 24.1% 2.4% 25.7 8.9
CBRC0048 22 23 151 15.2 10.1 3.1 15.0 3.1 138.8 1.4 92 27.8 16.8 2.4 1.5 103.4 9.1 590 440 426 164 27.8% 20.3% 2.6% 31.8 6.2
CBRC0048 23 24 176 15.7 8.5 4.3 19.7 2.9 204.1 1.1 136 40.8 24.0 2.9 1.2 84.3 7.6 729 553 581 148 20.3% 24.3% 2.2% 35.0 7.0
CBRC0048 24 25 154 14.0 8.2 3.4 16.1 2.7 124.1 1.1 98 28.0 18.1 2.4 1.1 87.0 6.9 566 412 423 143 25.3% 22.4% 2.5% 31.7 7.0
CBRC0048 25 26 77 11.7 8.8 1.7 9.6 2.7 57.5 1.2 39 11.2 8.1 1.7 1.2 104.8 7.5 344 267 194 151 43.8% 14.7% 3.4% 20.3 5.9
CBRC0048 26 27 177 23.5 17.4 3.2 19.6 5.6 93.5 2.1 75 21.3 15.4 3.4 2.2 237.1 13.2 710 533 382 327 46.1% 13.6% 3.3% 33.0 8.5
CBRC0048 27 28 107 10.4 7.8 1.7 9.6 2.4 55.2 0.9 43 12.3 8.2 1.6 1.0 112.1 5.6 378 271 225 153 40.5% 14.5% 2.7% 21.7 6.0
CBRC0048 28 29 95 9.0 6.3 1.6 8.1 2.0 50.5 0.7 42 12.0 8.0 1.4 0.8 78.3 4.9 321 226 208 113 35.3% 16.9% 2.8% 21.1 5.9
CBRC0048 29 30 175 10.2 6.4 2.2 10.8 2.1 74.6 0.7 68 19.3 12.2 1.7 0.9 69.4 5.1 459 284 349 109 23.9% 19.1% 2.2% 28.2 5.9
CBRC0048 30 31 157 10.2 6.6 2.1 10.3 2.1 73.5 0.8 64 18.5 11.8 1.7 0.9 73.4 5.4 438 281 325 113 25.9% 18.8% 2.3% 28.9 5.5
CBRC0048 31 32 90 5.5 3.6 1.2 5.5 1.2 41.6 0.5 37 10.8 6.8 0.9 0.5 39.7 3.2 248 158 186 62 24.9% 19.3% 2.2% 19.4 4.5
CBRC0048 32 33 104 5.5 3.9 1.4 6.0 1.2 47.3 0.5 42 12.3 7.9 0.9 0.5 42.0 3.2 279 175 214 65 23.4% 19.4% 2.0% 20.4 3.8
CBRC0048 33 34 179 7.6 3.8 2.2 9.6 1.4 73.9 0.4 69 20.2 12.5 1.4 0.5 41.6 3.2 427 247 355 72 16.8% 20.9% 1.8% 25.4 4.2
CBRC0048 34 35 148 7.0 3.5 1.9 8.7 1.3 68.3 0.4 63 18.1 11.4 1.3 0.5 38.0 2.8 374 226 309 65 17.5% 21.6% 1.9% 22.2 3.6
CBRC0048 35 36 101 5.5 2.9 1.5 6.2 1.0 53.6 0.4 45 13.2 8.3 1.0 0.4 31.3 2.7 274 173 221 53 19.3% 21.3% 2.0% 20.2 3.3
CBRC0048 36 37 123 7.3 3.7 2.0 9.1 1.3 64.0 0.4 64 17.8 11.9 1.3 0.5 36.1 3.1 345 223 281 65 18.8% 23.7% 2.1% 25.1 2.8
CBRC0048 37 38 88 5.7 3.1 1.4 6.3 1.1 35.9 0.4 38 10.5 7.5 1.0 0.5 31.8 3.0 234 146 180 54 23.2% 20.6% 2.4% 21.0 2.4
CBRC0048 38 39 63 4.7 3.5 0.9 4.2 1.1 24.6 0.5 25 6.7 4.6 0.7 0.5 36.6 3.4 179 117 123 56 31.2% 17.4% 2.6% 16.9 2.4
CBRC0048 39 40 99 9.3 6.2 1.7 9.8 2.0 37.9 0.8 39 10.0 7.9 1.5 0.9 65.1 5.4 297 198 194 103 34.6% 16.6% 3.1% 20.0 3.0
CBRC0048 40 41 104 8.1 4.8 1.8 9.1 1.6 58.9 0.6 49 13.5 9.4 1.4 0.7 49.8 4.3 317 213 234 82 26.0% 19.6% 2.6% 19.3 2.6
CBRC0048 41 42 100 5.7 3.7 1.3 6.4 1.2 52.7 0.5 43 12.1 7.6 0.9 0.5 37.1 3.3 276 176 215 61 22.0% 19.9% 2.1% 21.7 3.3
CBRC0048 42 43 114 8.7 6.0 1.9 9.4 1.9 60.9 0.8 55 15.2 10.3 1.4 0.9 64.2 5.4 357 242 256 101 28.2% 19.7% 2.4% 24.2 3.2
CBRC0048 43 44 155 10.7 5.8 2.6 12.5 2.0 78.1 0.7 74 19.8 14.2 1.9 0.8 59.1 5.0 442 287 341 101 22.9% 21.1% 2.4% 28.5 4.2
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0048 44 45 116 8.3 4.7 2.0 9.8 1.6 62.7 0.6 55 15.6 10.9 1.4 0.6 46.1 4.1 339 223 260 79 23.3% 20.8% 2.4% 26.1 4.8
CBRC0048 45 46 72 5.8 3.1 1.6 6.7 1.1 56.4 0.4 40 11.8 7.6 1.0 0.4 27.4 2.8 238 166 187 50 21.2% 21.6% 2.5% 20.9 4.2
CBRC0048 46 47 144 9.0 4.3 2.5 11.1 1.6 74.7 0.5 65 18.0 12.2 1.6 0.6 37.6 3.7 386 242 314 72 18.8% 21.4% 2.3% 21.5 3.8
CBRC0048 47 48 130 9.1 4.8 2.2 10.9 1.7 73.4 0.6 58 16.5 11.4 1.6 0.7 39.8 4.3 365 235 290 76 20.7% 20.5% 2.5% 20.4 3.4
CBRC0048 48 49 90 5.2 3.0 1.3 5.9 1.0 43.9 0.4 38 10.7 7.1 0.9 0.4 24.5 2.9 235 145 190 46 19.4% 20.5% 2.2% 19.8 3.9
CBRC0048 49 50 75 3.7 2.4 0.9 4.4 0.8 34.6 0.4 30 8.5 5.4 0.6 0.4 20.6 2.5 190 115 153 37 19.3% 20.2% 1.9% 21.5 4.4
CBRC0048 50 51 84 3.1 2.0 0.9 4.1 0.6 36.4 0.3 31 9.2 5.5 0.6 0.3 16.5 2.2 197 113 166 31 15.6% 20.6% 1.6% 20.4 5.2
CBRC0048 51 52 81 4.1 2.4 1.1 4.9 0.8 36.4 0.4 32 9.1 6.2 0.7 0.4 20.3 2.5 202 121 165 38 18.6% 20.4% 2.0% 20.0 6.2
CBRC0048 52 53 368 34.1 22.8 5.7 31.2 7.3 108.6 2.8 108 27.6 25.8 5.2 3.1 200.8 19.4 971 603 638 332 34.2% 14.0% 3.5% 21.7 5.7
CBRC0048 53 54 345 21.6 11.0 5.0 25.5 3.9 117.0 1.3 116 30.2 24.8 3.8 1.5 99.8 9.5 816 471 633 183 22.4% 17.9% 2.7% 24.1 7.5
CBRC0048 54 55 146 10.8 6.9 2.2 11.3 2.2 65.7 1.0 59 16.0 11.4 1.8 1.0 68.1 6.4 410 264 298 112 27.3% 18.2% 2.6% 23.2 6.3
CBRC0048 55 56 124 9.3 5.8 1.9 9.7 1.9 54.5 0.8 48 13.2 9.4 1.5 0.8 56.0 5.4 342 218 249 93 27.2% 17.8% 2.7% 16.2 6.6
CBRC0048 56 57 139 10.2 6.3 2.2 11.4 2.1 67.8 0.9 59 16.3 11.9 1.7 0.9 64.0 5.8 399 261 294 106 26.4% 18.9% 2.6% 22.7 7.2
CBRC0049 17 18 129 6.1 3.7 1.7 7.0 1.2 57.5 0.5 54 15.6 9.7 1.1 0.5 35.3 3.5 327 198 266 61 18.6% 21.5% 1.9% 23.1 6.0
CBRC0049 18 19 181 10.1 6.0 2.7 11.7 2.0 116.5 0.8 87 25.5 15.7 1.8 0.8 57.6 5.5 524 343 425 99 18.8% 21.5% 1.9% 23.6 6.6
CBRC0049 19 20 180 11.3 6.3 3.0 13.1 2.2 93.5 0.8 88 24.7 16.5 2.0 0.8 59.9 5.5 508 328 403 105 20.7% 22.2% 2.2% 20.8 6.1
CBRC0049 20 21 190 13.0 7.3 3.2 14.8 2.5 94.0 0.9 90 25.1 17.3 2.3 1.0 70.7 6.5 538 348 416 122 22.7% 21.3% 2.4% 22.7 5.8
CBRC0049 21 22 150 12.6 6.9 2.7 13.7 2.4 78.7 0.8 71 19.3 13.5 2.1 0.9 67.9 6.0 448 298 332 116 25.9% 20.1% 2.8% 23.7 4.8
CBRC0049 22 23 358 25.2 11.9 7.1 32.7 4.3 249.0 1.3 194 53.0 36.3 4.6 1.5 113.4 9.5 1,102 744 890 212 19.2% 22.4% 2.3% 22.2 7.6
CBRC0049 23 24 126 7.5 4.4 1.7 8.4 1.5 69.2 0.5 48 13.8 9.1 1.3 0.6 42.9 3.8 339 213 266 73 21.4% 18.3% 2.2% 17.3 4.8
CBRC0049 24 25 205 15.6 8.7 3.3 16.8 3.0 117.1 1.1 98 26.5 17.9 2.6 1.2 94.3 7.7 619 413 465 154 24.9% 20.0% 2.5% 22.9 4.7
CBRC0049 25 26 138 9.0 5.1 1.9 9.8 1.7 67.8 0.6 55 15.1 10.5 1.5 0.7 53.4 4.5 374 237 286 88 23.6% 18.8% 2.4% 18.2 4.3
CBRC0049 26 27 127 10.1 6.6 1.7 9.6 2.1 49.3 0.8 48 12.6 9.3 1.5 0.9 69.4 5.9 355 228 246 109 30.7% 17.0% 2.9% 21.1 3.8
CBRC0050 16 17 231 6.5 3.2 2.0 9.3 1.1 95.3 0.3 80 23.4 12.8 1.3 0.4 31.9 2.6 501 270 443 59 11.7% 20.6% 1.3% 43.0 3.4
CBRC0050 17 18 150 5.0 2.6 1.4 6.1 0.9 65.6 0.3 47 13.4 8.1 0.9 0.3 26.2 2.4 331 181 285 46 14.0% 18.4% 1.5% 27.3 3.3
CBRC0050 18 19 128 5.1 2.7 1.4 6.0 0.9 55.2 0.4 43 12.3 7.5 0.9 0.4 27.1 2.6 293 165 245 48 16.2% 18.8% 1.7% 21.9 3.7
CBRC0050 19 20 176 6.9 3.8 1.9 8.1 1.3 89.9 0.5 61 17.0 10.2 1.2 0.5 39.3 3.5 421 245 354 67 15.9% 18.4% 1.6% 20.7 3.8
CBRC0050 20 21 142 6.5 3.9 1.8 7.4 1.3 70.2 0.6 52 14.1 8.7 1.1 0.6 41.2 3.9 355 213 287 68 19.2% 18.6% 1.8% 18.1 2.7
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0050 51 52 138 5.4 3.2 1.6 6.5 1.0 62.7 0.5 51 13.4 8.6 1.0 0.5 31.0 3.2 327 189 274 54 16.4% 19.6% 1.7% 17.9 3.1
CBRC0050 52 53 336 9.5 5.0 3.1 12.7 1.7 150.8 0.7 123 35.5 18.7 1.7 0.7 49.8 4.7 754 417 664 90 11.9% 21.0% 1.3% 20.0 4.7
CBRC0050 53 54 142 7.3 4.2 1.8 8.4 1.4 60.7 0.6 49 13.6 8.8 1.3 0.6 40.8 4.1 344 202 274 70 20.5% 18.1% 2.1% 21.4 3.9
CBRC0050 54 55 168 5.5 3.4 1.7 7.1 1.1 79.4 0.5 63 17.5 10.0 1.0 0.5 35.7 3.1 397 229 338 60 15.0% 20.1% 1.4% 17.3 2.5
CBRC0051 15 16 287 11.6 4.6 3.9 15.1 1.9 109.8 0.5 114 33.9 22.1 2.2 0.6 40.0 3.5 651 364 567 84 12.9% 22.7% 1.8% 23.3 10.9
CBRC0051 16 17 342 16.9 7.1 4.7 20.9 2.9 153.9 0.7 139 39.7 25.7 3.1 0.9 65.4 5.4 828 486 700 128 15.5% 21.6% 2.0% 30.2 8.3
CBRC0051 17 18 149 8.8 4.2 2.1 9.9 1.6 69.4 0.5 58 16.4 11.0 1.5 0.6 40.6 3.5 377 228 303 73 19.5% 19.8% 2.3% 23.6 6.1
CBRC0051 18 19 198 11.3 5.8 3.1 12.8 2.0 193.0 0.8 82 27.2 16.2 2.0 0.8 53.0 5.3 613 415 516 97 15.8% 17.8% 1.8% 22.8 9.1
CBRC0051 19 20 883 43.2 18.3 11.9 51.4 7.5 483.1 1.6 312 91.9 58.4 7.5 2.2 177.6 12.5 2,162 1,279 1,828 334 15.4% 18.7% 2.0% 31.8 13.4
CBRC0051 20 21 278 15.4 9.6 3.5 16.7 3.3 130.9 1.3 101 29.5 18.0 2.5 1.3 113.0 8.1 732 454 557 175 23.9% 17.9% 2.1% 28.1 3.6
CBRC0051 21 22 229 9.1 5.1 2.2 10.5 1.8 103.0 0.7 72 21.2 12.5 1.5 0.7 56.7 4.4 531 302 438 93 17.5% 17.6% 1.7% 27.2 4.2
CBRC0051 22 23 125 7.7 4.2 2.1 9.2 1.5 83.6 0.5 60 17.6 11.1 1.3 0.6 44.9 3.6 373 248 298 76 20.3% 20.9% 2.1% 22.7 2.3
CBRC0052 18 19 172 6.2 3.2 1.8 7.5 1.1 60.3 0.4 57 15.7 10.1 1.1 0.5 29.9 2.8 369 197 315 54 14.8% 19.6% 1.7% 23.3 6.0
CBRC0052 19 20 212 8.7 4.4 2.4 10.4 1.6 85.1 0.5 74 20.6 13.2 1.6 0.6 43.8 3.6 482 271 405 78 16.1% 19.6% 1.8% 30.1 4.8
CBRC0052 20 21 210 9.1 4.6 2.6 11.3 1.6 94.4 0.5 82 23.1 14.3 1.7 0.6 45.5 3.6 505 295 424 81 16.1% 20.9% 1.8% 37.3 4.8
CBRC0052 21 22 190 8.9 4.3 2.4 10.7 1.5 91.6 0.5 72 20.4 13.0 1.6 0.6 44.4 3.4 466 275 387 78 16.8% 19.8% 1.9% 30.0 4.0
CBRC0052 22 23 210 9.8 5.2 2.6 11.8 1.8 101.2 0.6 83 23.3 15.0 1.8 0.7 53.0 4.0 524 314 433 91 17.4% 20.3% 1.9% 33.6 3.8
CBRC0052 23 24 207 10.4 5.4 2.7 11.8 1.9 93.6 0.6 80 21.8 14.4 1.8 0.8 54.4 4.4 511 304 417 94 18.4% 20.0% 2.0% 30.0 5.3
CBRC0052 24 25 171 9.8 5.2 2.5 10.8 1.8 77.0 0.6 67 18.5 12.5 1.7 0.7 53.2 4.1 437 266 346 91 20.7% 19.6% 2.2% 23.5 5.5
CBRC0052 25 26 182 9.8 5.2 2.4 10.7 1.8 78.6 0.6 70 19.2 13.0 1.7 0.7 52.1 4.2 452 270 363 89 19.7% 19.6% 2.2% 24.4 5.4
CBRC0052 26 27 201 9.7 5.5 2.4 10.7 1.9 84.7 0.7 70 19.2 12.5 1.6 0.8 57.8 4.5 483 282 387 95 19.8% 18.5% 2.0% 23.6 4.9
CBRC0052 27 28 184 9.2 5.2 2.2 10.2 1.8 80.4 0.6 68 18.8 12.3 1.6 0.7 52.7 4.2 452 268 364 88 19.5% 19.3% 2.0% 24.3 4.9
CBRC0052 28 29 179 8.5 4.7 2.1 9.2 1.6 85.3 0.6 67 18.7 11.7 1.5 0.7 48.8 4.1 443 264 362 82 18.4% 19.3% 1.9% 20.8 4.4
CBRC0052 29 30 189 9.8 5.4 2.5 11.0 1.9 84.1 0.7 71 19.5 13.0 1.7 0.8 56.5 4.7 472 283 377 95 20.1% 19.3% 2.1% 24.3 4.6
CBRC0052 30 31 107 7.8 4.7 1.7 8.0 1.6 56.5 0.7 45 11.7 8.7 1.3 0.7 50.1 4.3 310 203 229 81 26.1% 18.3% 2.5% 17.9 4.7
CBRC0052 31 32 224 9.6 5.4 2.5 11.1 1.8 99.5 0.8 71 19.5 12.8 1.7 0.8 57.6 4.9 523 299 427 96 18.4% 17.3% 1.8% 23.8 6.2
CBRC0052 32 33 160 8.4 4.6 2.1 9.8 1.5 75.3 0.6 65 17.6 11.9 1.5 0.7 50.3 4.2 413 254 330 84 20.3% 20.0% 2.0% 26.2 5.9
CBRC0052 33 34 114 7.4 4.5 1.7 8.0 1.5 61.0 0.7 51 13.8 9.7 1.2 0.7 44.0 4.2 323 210 250 74 22.8% 20.1% 2.3% 20.7 5.8
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0052 34 35 125 9.3 5.9 1.9 9.5 1.9 66.1 0.9 55 15.1 10.5 1.5 0.9 63.9 5.5 373 248 272 101 27.1% 18.9% 2.5% 23.2 5.0
CBRC0052 35 36 132 7.6 4.5 1.8 8.5 1.5 67.0 0.7 58 15.4 10.1 1.3 0.7 46.4 4.1 359 227 282 77 21.5% 20.3% 2.1% 24.9 4.1
CBRC0052 36 37 163 11.1 6.2 2.4 12.0 2.1 84.8 0.9 66 17.6 12.5 1.9 0.9 64.6 5.5 452 289 345 108 23.8% 18.6% 2.5% 24.3 4.9
CBRC0052 37 38 184 15.1 9.5 3.0 15.5 3.1 102.2 1.4 78 20.5 15.0 2.5 1.4 107.4 8.4 567 383 400 167 29.5% 17.4% 2.7% 26.9 5.6
CBRC0052 38 39 110 8.4 5.0 1.6 8.7 1.7 55.4 0.8 47 12.8 9.5 1.4 0.8 52.4 4.8 320 210 235 86 26.7% 18.7% 2.6% 29.5 4.5
CBRC0052 39 40 132 8.3 4.9 1.8 9.5 1.6 68.4 0.7 57 15.4 10.3 1.4 0.7 51.5 4.3 368 236 283 85 23.1% 19.7% 2.3% 27.4 4.9
CBRC0052 40 41 119 9.8 6.3 2.0 10.2 2.1 59.9 0.9 51 13.8 10.3 1.6 0.9 67.8 5.5 361 242 254 107 29.7% 18.0% 2.7% 24.3 3.6
CBRC0052 41 42 129 15.3 11.4 2.3 12.7 3.5 72.1 1.9 60 15.9 11.4 2.2 1.8 127.4 10.9 478 349 289 189 39.6% 15.9% 3.2% 23.7 4.9
CBRC0053 13 14 160 6.0 2.9 1.3 7.6 1.0 63.6 0.4 60 16.9 10.3 1.1 0.4 28.0 2.7 362 202 311 51 14.2% 21.2% 1.7% 24.3 3.1
CBRC0053 14 15 214 8.2 4.5 2.1 10.4 1.5 85.9 0.6 81 22.7 13.9 1.5 0.6 43.0 4.1 494 280 418 76 15.5% 21.0% 1.7% 25.7 2.9
CBRC0053 15 16 138 5.1 2.8 1.5 6.5 1.0 55.2 0.4 53 14.9 9.0 0.9 0.4 26.8 2.7 318 180 270 48 15.1% 21.2% 1.6% 20.4 4.2
CBRC0053 16 17 145 5.3 2.8 1.4 6.7 1.0 59.4 0.4 55 15.8 9.6 1.0 0.4 26.9 2.8 334 189 286 49 14.6% 21.2% 1.6% 22.3 4.1
CBRC0053 17 18 250 8.7 5.1 2.4 10.7 1.6 102.3 0.8 95 27.2 16.2 1.6 0.8 43.0 5.3 571 321 490 80 14.0% 21.4% 1.5% 26.0 5.1
CBRC0053 18 19 261 11.0 6.7 2.8 13.1 2.1 101.6 1.0 106 29.1 18.9 1.9 1.1 55.9 7.0 619 358 516 103 16.6% 21.8% 1.8% 30.1 7.1
CBRC0053 19 20 175 12.1 7.3 2.2 13.2 2.4 74.5 1.0 74 19.5 14.4 2.1 1.1 74.9 6.6 481 306 358 123 25.6% 19.5% 2.5% 27.5 6.5
CBRC0053 20 21 140 8.9 6.6 1.4 9.0 2.0 64.5 1.1 55 15.0 9.8 1.5 1.1 63.7 7.1 387 246 284 102 26.5% 18.0% 2.3% 25.0 4.3
CBRC0053 21 22 131 5.1 2.5 1.0 6.8 0.9 59.1 0.4 50 14.0 8.8 1.0 0.4 26.0 2.4 310 179 263 46 15.0% 20.8% 1.6% 27.0 3.0
CBRC0053 22 23 159 5.3 2.6 1.0 8.2 0.9 73.0 0.4 60 16.7 10.4 1.3 0.3 26.0 2.4 367 208 319 49 13.2% 20.8% 1.5% 28.8 3.1
CBRC0053 23 24 175 5.6 2.7 1.0 8.5 1.0 80.1 0.4 65 18.4 11.3 1.2 0.4 26.8 2.6 400 225 350 50 12.6% 20.9% 1.4% 32.3 3.1
CBRC0053 24 25 136 4.5 2.6 0.9 6.5 0.9 62.9 0.5 52 14.5 8.9 0.9 0.4 24.9 2.8 319 183 275 45 14.0% 21.0% 1.4% 26.3 2.6
CBRC0054 18 19 509 4.9 2.5 1.3 5.4 0.9 192.8 0.4 66 26.6 9.1 0.8 0.4 21.0 2.5 843 334 803 40 4.7% 10.9% 0.6% 53.8 11.2
CBRC0054 19 20 224 1.9 1.3 0.3 1.4 0.4 13.2 0.3 11 3.3 1.9 0.3 0.2 9.4 1.8 270 46 253 17 6.4% 5.1% 0.7% 37.4 10.5
CBRC0054 20 21 249 2.9 1.7 0.6 2.8 0.5 25.2 0.3 21 6.2 3.8 0.5 0.3 13.9 2.0 330 82 305 26 7.7% 8.2% 0.9% 47.9 19.2
CBRC0054 21 22 431 11.6 5.4 3.0 14.7 2.1 148.9 0.7 123 36.3 20.8 2.1 0.8 51.3 4.9 857 426 760 97 11.3% 18.6% 1.4% 72.5 22.5
CBRC0054 22 23 918 9.6 4.4 2.7 13.0 1.7 153.4 0.5 107 31.8 17.6 1.7 0.6 43.0 3.7 1,309 391 1,229 81 6.2% 10.6% 0.7% 68.7 31.1
CBRC0054 23 24 677 8.5 4.2 2.1 9.5 1.5 63.8 0.6 65 18.6 12.9 1.5 0.6 35.6 4.0 906 229 838 68 7.5% 9.3% 0.9% 60.4 25.2
CBRC0054 24 25 488 11.2 5.6 3.1 14.6 2.1 130.7 0.8 115 32.8 20.5 2.0 0.8 51.9 5.3 885 397 787 97 11.0% 16.8% 1.3% 46.5 14.4
CBRC0054 25 26 692 26.6 13.0 7.5 33.9 4.8 269.3 1.7 261 75.0 47.2 4.7 1.9 115.2 11.7 1,566 874 1,345 221 14.1% 21.5% 1.7% 54.0 15.7
Hole ID From (m) To (m) CeO2 Dy2O3 Er2O3 Eu2O3 Gd2O3 Ho2O3 La2O3 Lu2O3 Nd2O3 Pr6O11 Sm2O3 Tb2O3 Tm2O3 Y2O3 Yb2O3 TREO TREO - Ce LREO HREO % HREO %NdPr %Dy2O3 Th ppm U ppm
CBRC0054 26 27 390 75.3 35.8 21.0 99.8 13.4 716.1 4.0 698 195.9 126.0 14.0 4.9 353.6 28.9 2,776 2,386 2,125 651 23.4% 32.2% 2.7% 54.4 16.4
CBRC0054 27 28 308 25.5 15.3 5.4 33.1 5.4 356.9 1.7 181 50.7 29.8 4.3 2.0 203.9 10.9 1,234 926 926 308 24.9% 18.8% 2.1% 51.5 15.6
CBRC0054 28 29 228 8.6 4.2 2.3 10.6 1.6 111.9 0.5 79 23.3 13.7 1.6 0.6 42.1 3.5 531 303 455 76 14.2% 19.3% 1.6% 42.9 10.1
CBRC0054 29 30 395 17.8 9.0 4.5 22.2 3.3 208.8 1.1 159 45.7 27.6 3.2 1.3 90.6 7.4 996 601 836 160 16.1% 20.6% 1.8% 89.5 15.8
CBRC0054 30 31 329 12.2 5.8 3.3 15.6 2.2 141.1 0.7 116 34.1 20.8 2.3 0.8 56.6 4.7 745 416 641 104 14.0% 20.2% 1.6% 71.6 15.7
CBRC0054 31 32 302 14.9 7.0 3.8 18.3 2.6 167.5 0.9 129 36.6 22.7 2.6 1.0 74.2 5.6 789 487 658 131 16.6% 21.0% 1.9% 57.0 15.0
CBRC0054 32 33 295 12.0 5.6 3.3 15.2 2.1 144.4 0.6 112 31.9 19.7 2.1 0.8 57.8 4.6 707 412 603 104 14.7% 20.3% 1.7% 47.4 12.3
CBRC0054 33 34 190 9.5 5.2 2.5 10.4 1.8 92.3 0.7 67 19.3 12.3 1.6 0.8 53.6 5.0 473 282 382 91 19.3% 18.3% 2.0% 27.9 13.6
CBRC0054 34 35 177 7.8 4.4 2.0 8.4 1.5 88.4 0.7 57 17.0 10.0 1.3 0.7 43.2 4.3 424 247 350 74 17.5% 17.5% 1.8% 23.0 14.0
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