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RNS Number : 2512U Strategic Minerals PLC 25 February 2026
The information contained within this announcement is deemed by the Company to
constitute inside information as stipulated under the Market Abuse Regulations
(EU) No. 596/2014 ('MAR') which has been incorporated into UK law by the
European Union (Withdrawal) Act 2018.
25 February 2026
Strategic Minerals plc
("Strategic Minerals" or the "Company")
Redmoor - Positive Drill Results from Underexplored Western Portion of SVS
Strategic Minerals plc (AIM: SML; USOTC: SMCDF), an international mineral
exploration and production company, announces that its wholly owned
subsidiary, Cornwall Resources Limited ("CRL"), has received assay results
from drillhole CRD041 from the Redmoor Tungsten-Tin-Copper Project ("Redmoor")
in southeast Cornwall.
Results confirm the continuity of the Sheeted Vein System ("SVS") containing
high-grade tungsten- and tin-dominant mineralisation, with copper and silver
mineralisation also present, in the westward extent of the 2019 Redmoor JORC
(2012) Redmoor Mineral Resource. Results also confirm the presence of
additional non-SVS mineralised zones to the north of the SVS.
The western portion of the Redmoor deposit, more distal from the granite,
forms a zone containing a higher proportion of tin-dominant, rather than
tungsten-dominant, mineralisation with higher grades of tin. By comparison,
the eastern and central portions of the deposit contain a higher proportion of
tungsten-dominant mineralisation with higher tungsten grades. The polymetallic
composition of the deposit adds value as shown by the WO(3).eq*(1)
calculations.
SVS Downhole Composite Intersections Highlights
Multiple higher-grade intervals within high-grade tungsten- or high-grade
tin-dominant structures including copper were identified with results,
including:
o 0.94% WO(3) and 0.46% Cu over 0.95m from 507.00 m*(2)
o 1.57% Sn and 1.55% Cu over 2.18m from 575.95 m
o 2.54% Sn and 3.38% Cu over 0.88m from 580.62 m
High-grade tungsten equivalent ("WO(3).eq") intersections from SVS-style and
lode-style structures containing tungsten, tin and copper mineralisation
within the SVS in the western portion of the resource (see Figure 1 & 2),
which is tin-dominant:
· 9.18m @ 0.52% Sn, 0.17% Cu & 0.06% WO(3) (0.53% WO(3).Eq) from
528.92 m, with
o 3.40m @ 1.00% Sn, 0.15% Cu & 0.02% WO(3) (0.89% WO3.Eq) from 531.25 m
o 1.35m @ 0.70% Sn, 0.31% Cu & 0.19% WO(3) (0.85% WO3.Eq) from 536.75 m
· 6.85m @ 0.28% Sn, 0.30% Cu & 0.11% WO(3) (0.42% WO(3).Eq) from
553.70 m, with
o 1.30m @ 0.11% Sn, 0.22% Cu & 0.45% WO(3) (0.60% WO3.Eq) from 553.70 m
o 1.00m @ 0.86% Sn, 0.47% Cu & 0.18% WO(3) (1.01% WO3.Eq) from 556.00 m
· 8.10m @ 0.50% Sn, 0.65% Cu & 0.25% WO(3) (0.84% WO(3).Eq) from
571.00 m, with
o 1.45m @ 0.26% Sn, 0.80% Cu & 0.86% WO(3) (1.29% WO3.Eq) from 571.00 m
o 2.18m @ 1.57% Sn, 1.55% Cu & 0.22% WO(3) (1.93% WO3.Eq) from 575.95 m
· 4.68m @ 0.66% Sn, 0.97% Cu & 0.03% WO(3) (0.83% WO(3).Eq) from
580.62 m, with
o 0.88m @ 2.54% Sn, 3.38% Cu & 0.01% WO(3) (3.00% WO3.Eq) from 580.62 m
o 1.17m @ 0.50% Sn, 0.75% Cu & 0.01% WO(3) (0.62% WO3.Eq) from 584.13 m
Non-SVS Downhole Intersections
· CRD041 intersected a new zone of non-SVS mineralisation with visible
cassiterite (see RNS: 01 December 2025) (see Figure 3). With a sample
intersect of 4.00m @ 0.25% Sn, 0.01% Cu from 476.00m, including:
o 2.00m @ 0.40% Sn, 0.02% Cu & 0.00 WO3 (0.34% WO3.Eq) from 478.00 m
· Further information on this newly identified, tin-dominant, non-SVS
zone will follow shortly, alongside modelling outputs which are expected to
define this zone
· CRD041 also intersected additional zones of mineralisation outside of
the current resource model, including two intervals containing tungsten, tin
and copper with silver(*1) intersections, returning grades of:
o 0.65m @ 0.22% WO(3), 0.24% Sn & 3.19% Cu (1.28% WO(3).Eq) also
containing 75.8g/t Ag from 191.85 m,
o 4.00m @ 0.17% WO(3), 0.11% Sn & 0.32% Cu (0.34% WO(3).Eq) also
containing 19.1g/t Ag*(3) from 197.00 m, and
Figure 1: Long section looking south of the 2019 SVS model (shown in gold),
showing the trace of CRD041. Also showing the updated granite model surface
(pink) at depth and other drillholes (black). Trace of CRD041 shown to pass
into the under-explored, tin-dominant, western portion of the SVS.
Dennis Rowland, CRL Managing Director, said:
"Drillhole CRD041 intersected the Redmoor SVS, in the western extent of the
current Mineral Resource, within an area of the deposit where the mineral
zonation has a higher proportion of tin-dominant high-grade zones. The
drillhole results contain multiple intersections of tungsten- and tin-dominant
mineralised zones from within the SVS, with these zones also classified as
high-grade on a tungsten equivalent basis.
Additional intersections within the non-SVS section of the drillhole indicate
the potential for further zones of mineralisation outside of the current MRE
which may, subject to further delineation, estimation and assessment of
Reasonable Prospects for Eventual Economic Extraction ("RPEEE"), support
future resource definition."
Mark Burnett, Strategic Minerals Executive Director, said:
"The 2025 drill programme at Redmoor has shown the high-grade nature of the
SVS deposit, as well as its zonation. With the structural shifts in global
metal prices, especially for tungsten and tin, Redmoor's multicommodity
composition has the potential to provide significant economic benefits.
The Company is on schedule to complete its Shared Prosperity Fund match
grant-funded activities by the end of Q1 2026, including the new Mineral
Resource Estimate and economics updates, which we expect will further
highlight the potential of Redmoor as one of the highest grade, undeveloped,
tungsten resources in Europe."
Detail of analytical results from CRD041
CRD041 (see Table 1, and Figure 1, 2 & 3) was the final drillhole from Pad
3 at Redmoor between October and December 2025. CRD039, the second last
drillhole, has been delayed at the laboratory due to additional QAQC checks,
but is expected to be reported shortly.
Table 1: Drillhole collar data for CRD041.
Pad Collar Orientation at Collar Total Depth (m)
Number
DH Easting (m) Northing (m) Elevation (m) Azimuth (⁰) Dip (⁰)
3 CRD041 235881.0 71305.0 187 180 85 602.40
Figure 2: Plan (top-down) view of the previously modelled high-grade domains
(shown in gold) used in the 2019 Redmoor MRE, showing CRD041 (red) and other
CRL and SWM drillhole traces (black).
Figure 3: Cross-sectional view of the updated model, showing high-grade
domains (red and green) identified during historical drilling, and CRD041
showing the mineralised continuity of these structures' westwards.
At the outset of the 2025 drilling campaign, the Company established several
key objectives, including confirmation of continuity of structure and grade
within the resource, verification of validity of the 1980s drillhole datasets,
and testing a portion of the Redmoor JORC Exploration Target. Each of these
targets have been met and are expected to both strengthen the deposit model
and produce significant benefits to future drilling programmes. A further
objective was to validate the potential presence of additional mineralised
structures outside of the Redmoor SVS, which could add to the current Mineral
Resource, subject to estimation. The results from CRD039 are expected shortly,
concluding the 2026 drilling programme.
As shown in Figure 2, the western, tin-dominant, extent of the deposit is less
explored by drilling than the eastern and central portions. CRD041's objective
was to identify the presence and continuity of SVS mineralisation within the
western portion of the deposit and to further identify and confirm the
presence of additional non-SVS mineralised zones as predicted by the current
geological model following the review of historical exploration data.
CRD041 successfully intersected the full section of the SVS (see Table 2).
This portion of the deposit is known to contain a greater proportion of
high-grade, tin-dominant zones when compared to the rest of the deposit - with
the central and eastern portions containing more higher-grade
tungsten-dominant zones (see Figure 3).
Historical drilling intersected mineralised intervals in this area outside of
the currently modelled Redmoor SVS resource. However, through drilling CRD041,
CRL was able to identify new structures hosting tin, tungsten and copper
mineralisation that were not previously delineated. This includes the newly
identified tin zone detailed in the highlights above. Following review of
historical datasets other structures with sample results have been identified,
with examples below.
Examples of historical intercepts located outside and north of the JORC (2012)
Redmoor 2019 Resource Model and are provided for context:
· RM82_24 (intersects not previously reported by CRL, data reviewed and
verified by Competent Person) containing:
o 0.70m @ 3.40% Sn and 0.71% Cu from 148.92 m
o 0.86m @ 0.47% Sn and 0.21% Cu from 288.34 m, and
o 2.00m @ 0.60% Sn and 0.24% Cu from 408.00 m.
· RM82_24A (intersects not previously reported by CRL, data reviewed
and verified by Competent Person) containing:
o 2.00m @ 0.38% Sn and 0.02% Cu from 252.00 m
o 2.00m @ 0.26% Sn and 0.03% Cu from 318.00 m
· CRD027 (results from reanalysis programme previously reported in RNS
03 December 2024, data reviewed and verified by Competent Person) containing:
o 1.00m @ 1.33% Sn, 0.01% WO(3) & 0.02% Cu from 255.03 m
o 1.00m @ 0.39% Sn and 0.11% Cu from 354.10 m, and
o 1.00m @ 2.56% Sn, 1.49% WO(3) & 0.09% Cu from 371.35 m
· CRD029 (results from reanalysis programme previously reported in RNS
02 August 2024, data reviewed and verified by Competent Person) containing:
o 1.06m @ 0.13% Sn, 0.21% WO(3) & and 0.10% Cu from 295.34 m
o 1.00m @ 0.98% Sn and 0.10% Cu from 352.06 m,
o 1.24m @ 0.84% Sn and 0.06% Cu from 364.27 m,
o 1.00m @ 5.13% Sn and 0.01% Cu from 366.51 m,
o 2.00m @ 0.48% Sn and 0.13% Cu from 381.50 m,
o 1.00m @ 0.96% Sn and 0.01% Cu from 416.82 m
Table 2: Highlights of downhole composite sample intersections returned from
recently received results from drillhole CRD041 showing interval lengths and
subsequent assay results for WO3, Sn & Cu. A tungsten equivalent result
has also been calculated(*2). Composited values use a downhole length weighted
average of grades.
Sample Start From (m) To (m) Interval (m) WO3 % Cu % Sn % WO3 eq. % Comments
New Zones of Mineralisation Outside Redmoor SVS
CRL006795 191.85 192.5 0.65 0.22 3.19 0.24 1.28 S.V.S Mineralisation
CRL006799-01 197.00 201.00 4.00 0.17 0.32 0.11 0.34 S.V.S Mineralisation
incl. CRL006799 197.00 199.00 2.00 0.32 0.15 0.13 0.47 S.V.S Mineralisation
CRL006828-31 476.00 480.00 4.00 0.00 0.01 0.25 0.22 Lode-Style Sn Mineralisation
incl. CRL006831 478.00 480.00 2.00 0.00 0.02 0.40 0.34 Lode-Style Sn Mineralisation
Redmoor SVS Mineralisation
CRL006843 500.00 502.00 2.00 0.05 0.04 0.32 0.32 Lode-Style Sn Mineralisation
CRL006845-48 504.00 509.00 5.00 0.20 0.29 0.11 0.36 S.V.S Mineralisation
incl. CRL006847 507.00 507.95 0.95 0.94 0.46 0.08 1.13 S.V.S Mineralisation
CRL006854-55 513.07 517.00 3.93 0.03 0.10 0.41 0.39 Lode-Style Sn Mineralisation
incl. CRL006854 513.07 515.00 1.93 0.03 0.17 0.59 0.56 Lode-Style Sn Mineralisation
CRL006859 523.00 524.38 1.38 0.00 0.12 0.90 0.77 Lode-Style Sn Mineralisation
CRL006865-74 528.92 538.10 9.18 0.06 0.17 0.52 0.53 S.V.S Mineralisation
incl. CRL006867-71 531.25 534.65 3.40 0.02 0.15 1.00 0.89 S.V.S Mineralisation
incl. CRL006874 536.75 538.10 1.35 0.19 0.31 0.70 0.85 S.V.S Mineralisation
CRL006879-82 545.00 549.00 4.00 0.02 0.29 0.23 0.29 Lode-Style Cu+Sn Mineralisation
incl. CRL006879 545.00 546.00 1.00 0.00 0.88 0.78 0.88 Lode-Style Cu+Sn Mineralisation
CRL006884-85 550.05 552.20 2.15 0.04 0.18 0.14 0.21 Lode-Style Cu+Sn Mineralisation
incl. CRL006884 550.05 550.95 0.90 0.00 0.22 0.28 0.29 Lode-Style Cu+Sn Mineralisation
CRL006887-94 553.70 560.55 6.85 0.11 0.30 0.28 0.42 S.V.S Mineralisation
incl. CRL006887 553.70 555.00 1.30 0.45 0.22 0.11 0.60 S.V.S Mineralisation
incl. CRL006891 556.00 557.00 1.00 0.18 0.47 0.86 1.01 S.V.S Mineralisation
CRL006896-99 561.42 564.00 2.58 0.12 0.27 0.17 0.33 S.V.S Mineralisation
CRL006907-16 571.00 579.10 8.10 0.25 0.65 0.50 0.84 S.V.S Mineralisation
incl. CRL006907 571.00 572.45 1.45 0.86 0.80 0.26 1.29 S.V.S Mineralisation
incl. CRL006914-15 575.95 578.13 2.18 0.22 1.55 1.57 1.93 S.V.S Mineralisation
CRL006918-23 580.62 585.30 4.68 0.03 0.97 0.66 0.83 S.V.S Mineralisation
incl. CRL006918 580.62 581.50 0.88 0.01 3.38 2.54 3.00 S.V.S Mineralisation
incl. CRL006923 584.13 585.30 1.17 0.01 0.75 0.50 0.62 S.V.S Mineralisation
CRL006925-27 587.00 591.00 4.00 0.13 0.29 0.15 0.33 S.V.S Mineralisation
incl. CRL006925 587.00 588.10 1.10 0.42 0.36 0.07 0.58 S.V.S Mineralisation
CRL006933 595.00 596.00 1.00 0.10 0.16 0.12 0.24 S.V.S Mineralisation
Note(1) Tungsten Equivalent (WO(3).Eq) Calculation: WO₃ (EQ)% = WO₃%+(Sn%
x 0.82) + (Cu% x 0.27)
Commodity price assumptions: WO₃ US$ 43,000/t, Sn US$ 32,525/t, Cu US$
9,429/t. Using the 12-month average to September 2025. Recovery assumptions:
total WO₃ recovery 72%, total Sn recovery 68% and total Cu recovery 85%.
Payability assumptions of 81%, 90% and 90% respectively.
Note*(2) Depths are downhole, not vertical depth, and longer due to the more
northerly collar location of Pad 3.
Note*(3) Further silver analysis and commentary will follow completion of
metallurgical testworks and resource modelling, noting there is no assumption
at this stage that silver will be recoverable or economically reportable in
the Mineral Resource.
Competent Person Statement:
The information in this announcement that relates to Sampling Techniques and
Data and Exploration Results has been reviewed and approved by Mr Laurie
Hassall, MSci (Geology), FIMMM, QMR, FGS, who is a full-time employee of
Snowden Optiro. Mr Hassall holds a Master of Science degree in Geology from
the University of Southampton and is a Fellow of the Institute of Materials,
Minerals and Mining (FIMMM), through which he is also accredited as Qualified
for Minerals Reporting (QMR). He is also a Fellow of the Geological Society of
London (FGS).
Snowden Optiro has been engaged by Cornwall Resources Limited to provide
independent technical advice. Mr Hassall, a full-time employee of Snowden
Optiro, is acting as the Competent Person and is independent of Cornwall
Resources Limited. He has sufficient experience that is relevant to the style
of mineralisation and type of deposit under consideration, and to the activity
being undertaken, to qualify as a Competent Person as defined in the 2012
Edition of the Australasian Code for Reporting of Exploration Results, Mineral
Resources and Ore Reserves (JORC Code), and under the AIM Rules.
Mr Hassall consents to the inclusion in this announcement of the matters based
on his information, in the form and context in which it appears. He confirms
that, to the best of his knowledge, there is no new information or data that
materially affects the information contained in previous market announcements,
and that the form and context in which the information is presented has not
been materially modified.
For further information, please contact:
Strategic Minerals plc +44 (0) 207 389 7067
Mark Burnett
Executive Director
Website: www.strategicminerals.net (http://www.strategicminerals.net)
Email: info@strategicminerals.net (mailto:info@strategicminerals.net)
Follow Strategic Minerals on:
X: @StrategicMnrls (https://x.com/StrategicMnrls)
LinkedIn: https://www.linkedin.com/company/strategic-minerals-plc
(https://www.linkedin.com/company/strategic-minerals-plc)
SP Angel Corporate Finance LLP +44 (0) 20 3470 0470
Nominated Adviser and Broker
Matthew Johnson/Charlie Bouverat/Grant Barker +44 (0) 203 829 5000
Zeus Capital Limited
Joint Broker
Harry Ansell/Katy Mitchell
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Investor Relations
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Email: strategicminerals@vigoconsulting.com
(mailto:strategicminerals@vigoconsulting.com)
Notes to Editors
About Strategic Minerals plc and Cornwall Resources Limited
Strategic Minerals plc (AIM: SML; USOTC: SMCDY) is an AIM-quoted, producing
minerals company, actively developing strategic projects in the UK, United
States and Australia.
In 2019, the Company completed the 100% acquisition of Cornwall Resources
Limited and the Redmoor Tungsten-Tin-Copper Project.
The Redmoor Project is situated within the historically significant Tamar
Valley Mining District in Cornwall, United Kingdom, with a JORC (2012)
Compliant Inferred Mineral Resource Estimate published 14 February 2019:
Cut-off (SnEq%) Tonnage (Mt) WO(3) Sn Cu Sn Eq(1) WO(3) Eq
% % % % %
>0.45 <0.65 1.50 0.18 0.21 0.30 0.58 0.41
>0.65 10.20 0.62 0.16 0.53 1.26 0.88
Total Inferred Resource 11.70 0.56 0.16 0.50 1.17 0.82
1 Equivalent metal calculation notes; Sn(Eq)% = Sn% x 1 + WO3% x 1.43 + Cu% x
0.40. WO(3)(EQ)% = Sn% x 0.7 + WO(3) + Cu% x 0.28. Commodity price
assumptions: WO₃ US$ 33,000/t, Sn US$ 22,000/t, Cu US$ 7,000/t. Recovery
assumptions: total WO3 recovery 72%, total Sn recovery 68% & total Cu
recovery 85% and payability assumptions of 81%, 90% and 90% respectively
More information on Cornwall Resources can be found at:
https://www.cornwallresources.com (https://www.cornwallresources.com)
In September 2011, Strategic Minerals acquired the distribution rights to the
Cobre magnetite project in New Mexico, USA, through its wholly owned
subsidiary Southern Minerals Group. Cobre has been in production since 2012
and continues to provide a sustainable revenue stream for the Company.
In March 2018, the Company completed the acquisition of the Leigh Creek Copper
Mine situated in the copper rich belt of South Australia. The Company has
entered into an exclusive Call Option with South Pacific Mineral Investments
Pty Ltd trading as Cuprum Metals to acquire 100% of the project.
About the CIOS Good Growth Fund and UK Shared Prosperity Fund
This project is part-funded by the UK Government through the UK Shared
Prosperity Fund. Cornwall Council is responsible for managing projects
funded by the UK Shared Prosperity Fund through the Cornwall and the Isles of
Scilly Good Growth Programme (https://ciosgoodgrowth.com/) .
Cornwall and Isles of Scilly has been allocated £184 million for local
investment through the Shared Prosperity Fund
(https://www.gov.uk/government/publications/uk-shared-prosperity-fund-prospectus/uk-shared-prosperity-fund-prospectus)
. This new approach to investment is designed to empower local leaders and
communities, so they can make a real difference on the ground where it's
needed the most.
The UK Shared Prosperity Fund proactively supports delivery of the
UK-government's five national missions: pushing power out to communities
everywhere, with a specific focus to help kickstart economic growth and
promoting opportunities in all parts of the UK.
For more information, visit
https://www.gov.uk/government/publications/uk-shared-prosperity-fund-prospectus
(https://www.gov.uk/government/publications/uk-shared-prosperity-fund-prospectus)
For more information, visit https://ciosgoodgrowth.com
(https://ciosgoodgrowth.com)
Appendix 1
Table 3: Composite intersections and individual sample results, including,
sample numbers, depths and widths, metal contents and tungsten equivalent
calculations.
Sample Start From (m) To (m) Interval (m) WO3 % Cu % Sn % WO3 eq. %
CRL006795 191.85 192.5 0.65 0.22 3.19 0.24 1.28
CRL006799-01
CRL006799 197.00 199.00 2.00 0.32 0.15 0.13 0.47
CRL006801 199.00 201.00 2.00 0.01 0.50 0.09 0.22
CRL006828-31
CRL006828 476.00 478.00 2.00 0.01 0.01 0.11 0.09
CRL006831 478.00 480.00 2.00 0.00 0.02 0.40 0.34
CRL006843 500.00 502.00 2.00 0.05 0.04 0.32 0.32
CRL006845-48
CRL006845 504.00 506.00 2.00 0.01 0.21 0.11 0.16
CRL006846 506.00 507.00 1.00 0.05 0.24 0.03 0.14
CRL006847 507.00 507.95 0.95 0.94 0.46 0.08 1.13
CRL006848 507.95 509.00 1.05 0.01 0.35 0.20 0.27
CRL006854-55
CRL006854 513.07 515.00 1.93 0.03 0.17 0.59 0.56
CRL006855 515.00 517.00 2.00 0.03 0.02 0.23 0.22
CRL006859 523.00 524.38 1.38 0.00 0.12 0.90 0.77
CRL006865-74
CRL006865 528.92 530.00 1.08 0.08 0.13 0.06 0.16
CRL006866 530.00 531.25 1.25 0.06 0.24 0.05 0.17
CRL006867 531.25 532.20 0.95 0.01 0.19 0.18 0.21
CRL006868 532.20 533.70 1.50 0.05 0.20 2.01 1.75
CRL006871 533.70 534.65 0.95 0.01 0.05 0.24 0.22
CRL006872 534.65 535.82 1.17 0.00 0.01 0.01 0.01
CRL006873 535.82 536.75 0.93 0.01 0.18 0.32 0.33
CRL006874 536.75 538.10 1.35 0.19 0.31 0.70 0.85
CRL006879-82
CRL006879 545.00 546.00 1.00 0.00 0.88 0.78 0.88
CRL006881 546.00 547.88 1.88 0.00 0.02 0.00 0.01
CRL006882 547.88 549.00 1.12 0.07 0.22 0.12 0.23
CRL006884-85
CRL006884 550.05 550.95 0.90 0.00 0.22 0.28 0.29
CRL006885 550.95 552.20 1.25 0.07 0.16 0.05 0.15
CRL006887-94
CRL006887 553.70 555.00 1.30 0.45 0.22 0.11 0.60
CRL006889 555.00 556.00 1.00 0.01 0.20 0.16 0.20
CRL006891 556.00 557.00 1.00 0.18 0.47 0.86 1.01
CRL006892 557.00 558.00 1.00 0.00 0.31 0.28 0.31
CRL006893 558.00 559.25 1.25 0.00 0.28 0.26 0.29
CRL006894 559.25 560.55 1.30 0.00 0.35 0.11 0.19
CRL006896-98
CRL006896 561.42 562.00 0.58 0.01 0.47 0.49 0.54
CRL006898 562.00 563.00 1.00 0.00 0.05 0.01 0.03
CRL006899 563.00 564.00 1.00 0.29 0.37 0.14 0.50
CRL006907-16
CRL006907 571.00 572.45 1.45 0.86 0.80 0.26 1.29
CRL006908 572.45 573.00 0.55 0.00 0.02 0.00 0.01
CRL006911 573.00 574.05 1.05 0.29 0.27 0.03 0.38
CRL006912 574.05 575.00 0.95 0.01 0.14 0.03 0.07
CRL006913 575.00 575.95 0.95 0.02 0.24 0.18 0.23
CRL006914 575.95 576.90 0.95 0.01 0.71 1.81 1.68
CRL006915 576.90 578.13 1.23 0.39 2.20 1.39 2.12
CRL006916 578.13 579.10 0.97 0.00 0.10 0.02 0.05
CRL006918-23
CRL006918 580.62 581.50 0.88 0.01 3.38 2.54 3.00
CRL006919 581.50 582.34 0.84 0.02 0.03 0.03 0.05
CRL006921 582.34 583.23 0.89 0.10 0.72 0.23 0.49
CRL006922 583.23 584.13 0.90 0.00 0.06 0.02 0.03
CRL006923 584.13 585.30 1.17 0.01 0.75 0.50 0.62
CRL006925-27
CRL006925 587.00 588.10 1.10 0.42 0.36 0.07 0.58
CRL006926 588.10 589.70 1.60 0.01 0.16 0.06 0.10
CRL006927 589.70 591.00 1.30 0.02 0.40 0.33 0.40
CRL006933 595.00 596.00 1.00 0.10 0.16 0.12 0.24
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