Churchill Intersects 19.23% Antimony over 1.40 metres at Frost Cove North and at PC Pond Expands Vein Swarm and Intersects New Prospect Grading 0.78% Copper with 61.2 g/t Silver over 6.22 metres on the Black Raven Project, Central Newfoundland
Churchill Intersects 19.23% Antimony over 1.40 metres at Frost Cove North and at PC Pond
Expands Vein Swarm and Intersects New Prospect Grading 0.78% Copper with 61.2 g/t
Silver over 6.22 metres on the Black Raven Project, Central Newfoundland
TORONTO, ON / ACCESS Newswire / August 28, 2026 / Churchill Resources Inc. (“Churchill” or
the “Company”) (TSXV: CRI.V) is pleased to report final assay results from its Spring 2026 program
of core drilling and trenching at the Black Raven Project. The work was focused on both Pomley Cove
Pond (“PC Pond”) where the Company’s recent discovery of a potentially extensive polymetallic vein
swarm associated with rhyolitic volcanic rocks has been significantly expanded, and a second round
of delineation drilling of the Frost Cove North antimony-gold prospect.
The Spring program included the drilling of 23 drillholes, with a cumulative depth of 4,267m (Table 5),
along with extensive trenching, channel , and soil sampling. Fourteen holes, totalling 2,9 79m depth,
were dedicated to expanding the PC Pond prospect (Fig. 1, Tables 1-3), and the remaining nine holes
(cumulative of 1288m) to delineation work at Frost Cove North (Fig. 2, Table 4) ; all results reported
here. Most holes were surveyed by televiewer to assist with Leapfrog modelling of the PC Pond
complex and refining the Frost Cove North geological model.
At PC Pond , the 2026 drilling both expanded the Au -Ag-Mo vein swarm and discovered a broad
succession of associated felsic extrusive rocks first intersected in hole PC25 -02, within the down-
dropped portion of a regional graben structure, that appears to be at, or near, the locus of the Black
Raven mineralization and quartz -feldspar porphyry dykes . A delineation drilling program for the Fall
on the Peninsula Vein Swarm (“PVS”) is being planned, to target the strike extents of, and drill the first
deep holes into, the mineralized structure.
At Frost Cove North the highlight was drillhole FC26-34, targeted on a gap in our 2025 delineation
drilling, which intersected a project best 19.23% Sb and 0.73 gpt Au over 1.4 0m, which included an
interval of 56.20% Sb over 0.47m. The majority of the other holes intersected polymetallic Au-Ag-Sb-
As-Zn mineralization.
Churchill interprets these results as indic ating that the Black Raven Property potentially contains a
large-scale mineralized system in which critical and precious metals occur in association with felsic
intrusive (dyke) and extrusive (volcanic flow and breccia) rocks, all centred about PC Pond . The
Company is excited by our exploration results to date and doubled the 2025 soil sampling this Spring
to expand coverage at the mineralized core of the project.
PC Pond Gold, Silver, Molybdenum Spring 2026 Highlights Include:
• Mineralized Zones within Interpreted Felsic Volcanic Complex (Fig. 1, Tables 1-3, 5)
2026 PC Pond drilling intersected a newly recognized felsic volcanic complex that correlates
with historical IP (“induced polarization”) chargeability and arsenic-in-soil anomalies, due to its
elevated disseminated arsenopyrite content s. Numerous mineralized shear zones/quartz
veins were intersected within, and adjacent to, the dome per Fig 1. The Peninsula Vein Swarm
and Western Shear Zone are interpreted to be primary fault systems integral to the volcanic
complex.
• Expanded gold-silver-molybdenum vein system at the Peninsula Vein Swarm (“PVS”)
The original vein swarm discovery made in November 2025 has now been expanded to an
interpreted strike length of at least 200m along strike to the north, from the results of channels
in Trench TRPC-02 along the length of the peninsula , and from drillhole PC26-03 at its north
end. Systematic channels in the trench exposed numerous sulphide-rich shear zones within
2
both the mafic country rock as well as the brecciated felsic dome rocks carrying 1-5%
disseminated arsenopyrite. There is a distinct molybdenum enrichment, as well as potassic
and magnetite alteration evident in the centre of the PVS within numerous veins over the core
~100m width in plan-view of the structural corridor. The PVS is interpreted to potentially extend
hundreds of metres further to both the north and south and is open at depth where more ductile
rocks may have allowed for larger mineralizing systems to form. Elsewhere in the felsic dome
complex the alteration, volcanic textures, and isolated mineralized structures suggest a more
distal setting.
Highlights include:
o Surface (Tables 1 and 2): Intercepts include the following (weighted averages):
▪ 2.47 g/t Au, 78.8 g/t Ag over 1.58 m (TRPC02 – channel 20)
▪ 1.21 g/t Au, 51.3 g/t Ag, 918 ppm Mo over 0.57m (TRPC02 – channel 15)
o Drilling (Table 3 ): Hole PC26-03 was targeted to intersect the inferred strike of the
PVS approximately 200m to the north of the discoveries and it intersected a portion of
the overall structure. Hole PC26 -16 targeted to cross the structure ~100m south of
Hole PC26-03, intersected encouraging stockworkveining and visible molybden ite
mineralization further raising confidence in the PVS being an important fluid conduit.
The planned Fall 2026 drill program will commence with extending holes PC26-03 and
PC26-16 across the entirety of the PVS, followed by systematic delineation work along
strike.
o Intercepts in PC26-03 include the following (weighted averages):
▪ 3.68 g/t Au, 10.7 g/t Ag over 0.67m.
▪ Numerous discrete vein and breccia samples returned elevated Au, Ag , and
Mo assays throughout the 173m intersection of rhyolite.
o Intercepts in PC26-16 include the following (weighted averages):
▪ Numerous veins returned elevated Au, Ag, and Mo assays.
▪ Individual samples assayed high values of 1.67 gpt Au, 135 gpt Ag, 1.10% Pb,
2.28% Zn, and 787 ppm Mo.
▪ The best molybdenum intersection on the property was intersected near
surface, 1.09% Mo over 0.19m at 8.36m down hole (-45 degree dip).
• New Copper-Silver- Gold Prospect – Hole PC26-06 Intersection
▪ Drillhole PC26-06 was designed to test a strong arsenic-copper-gold-silver soil
anomaly with coincident IP chargeability response
▪ Strong chalcopyrite mineralization was intersected in a broad felsic breccia
grading 0.78% Cu, 61.2 gpt Ag, and 0.23 gpt Au over 6.22m
▪ Higher grading material included within the broader interval yielded 1.47%
Cu,120.0 gpt Ag, and 0.42 gpt Au over 2.66m.
▪ The planned Fall 2026 program will investigate this copper-silver-gold prospect
with trenching and drilling.
3
Figure 1 – Pomley Cove Pond Surface Sampling and Drilling Highlights to 25-08-26
4
Frost Cove North Antimony-Gold Prospect Spring 2026 Highlights Include:
• The 2026 program was designed to intersect the Antimony and Gold -Silver-
bearing shear zones along the northern 500m of the host structure at low
angles to assess the continuity of mineralization, and identify the location of
cross structures.
▪ Holes FC26-31 and 32 were designed to test the northern strike extent of the
historical mine and were successful with hole FC26-31 intersecting two
antimony zones with the lower interval grading 3.24% Sb and 0.39gpt Au over
0.74m. Hole FC26-32 drilled at a steeper dip along the same azimuth
intersected gold-silver-zinc mineralization per Figure 2 and Table 4.
▪ Hole FC26-34 was targeted on a gap in our 2025 delineation , ~50m north of
the historical shaft, and intersected a project-best 19.23% Sb and 0.73 gpt Au
over 1.40m.
▪ Holes FC26-35 to 39 did not intersect the antimony shear due to microgranite
intrusions along the host quartz-feldspar dyke which appear to have disrupted
or redirected the antimony-bearing shear on the east side of the dyke.
▪ Holes FC26-35 to FC26-37 did intersect the Au -Ag shear zone which carried
low antimony grades as well.
▪ Geological and mineralogical information from holes FC26 -31 to 39 will allow
for a more robust structural-geological Leapfrog model of Frost Cove North
▪ Detailed mapping is planned over Frost Cove South to better understand the
complex structural setting and thereby direct follow-up trenching where
massive stibnite mineralization has been found and traced for ~80m on
surface.
Note that all drill core and channel sample lengths and composite intervals provided in the tables, figures
and text in this news release are measured core/channel lengths and do not represent true thicknesses of
the units sampled.
Additional Black Raven Technical Activities
▪ Soil grid expanded to the west, south, and east - ~2600 soil samples to report
▪ Property-scale and detailed mapping/prospecting partially complete
▪ Leapfrog modelling of the PC Pond complex has commenced along with
updating the Frost Cove North geological model
5
Figure 2– Frost Cove North Drilling Results to 25-08-2026
About the Black Raven Gold-Silver-Antimony Project
The Black Raven Project is a polymetallic exploration asset in Central Newfoundland characterized by
high-tenor antimony mineralization and gold -silver-lead-zinc-molybdenum systems. Churchill's
primary objective is to evaluate the projects’ potential to host small-footprint, high-grade underground
mine(s).
The project encompasses the past -producing Frost Cove Antimony Mine and Stewart Gold Mine.
While these sites operate d intermittently at the turn of the last century, Churchill is the first to apply
modern systematic exploration techniques over the entire property to understand these and other
occurrences. Black Raven is located approximately 60km northwest of Gander, Newfoundland, and
approximately 100km north of the dormant Beaver Brook Antimony Mine. The project benefits from
excellent infrastructure, including roads, power, proximity to tidewater and ports, and locally integrated
operational and technical teams.
Antimony is recognized as a vital critical mineral, essential for Canada’s national and economic
security. It is a key component in military applications, flame retardants, alloy strengthening in
batteries, and emerging energy storage technologies. Securing a reliable domestic supply chain for
6
antimony is paramount for critical mineral supply chains, bolstering both economic resilience and
strategic independence. Currently, North America lacks sources of high -grade, primary antimony
supply, making a potential domestic source at Black Raven critically important.
About Churchill Resources
Churchill Resources Inc. is a Canadian exploration company focused on exploration and evaluation
of strategic and critical metals in Canada, principally at its prospective Black Raven, Golden Baie,
Taylor Brook and Florence Lake properties in Newfoundland & Labrador. The Churchill management
team and board have decades of combined experience in mineral exploration and in the establishment
of successful publicly listed mining companies, both in Canada and around the world. Churchill’s
Newfoundland and Labrador projects benefit from the province’s large and di versified minerals
industry, which includes tier-one class mines and processing facilities, and a well -developed mineral
exploration sector with locally based drilling and geological expertise.
Qualified Person
The technical and scientific information in this news release has been reviewed and approved by Dr.
Derek H.C Wilton, P.Geo., FGC, who is a “qualified person” as defined under National Instrument 43-
101 – Standards of Disclosure for Mineral Projects (“NI 43-101”). Dr. Wilton is a former professor of
Economic Geology at Memorial University in St. John’s and is independent of the Company for the
purposes of NI 43 -101. Dr. Derek Wilton has examined all of the grab and channel sampling sites
and all drill holes reported herein. Dr. Wilton is included on all assay reports from the laboratories and
has total access to the Company’s cloud-based central database for data validation purposes.
Sampling Program
Antimony, gold, silver, lead, zinc, copper and molybdenum samples were identified and collected by
Company geologists from drill cores, channel samples, and grab samples. Core samples were halved
by saw at the Company’s core facility near Boyd’s Cove. Trench and grab samples were entirely
submitted. Note that grab samples are selective in nature and therefore may not represent the true
grade of the outcrop sampled.
All samples were labelled and securely bound and delivered to the laboratory of Activation
Laboratories Ltd. (“Actlabs”) in Fredericton, New Brunswick, for crushing and pulverizing. Actlabs is
ISO/IEC 17025 (Lab 266) certified, Health Canada Licensed, FDA inspected and registered , and
independent of Churchill. Blanks and known standards for antimony and gold were included by
Company geologists both regularly every 20 samples, and also immediately following all high-grade
samples. Splits were couriered to Actlabs, Ancaster and analysed by using Actlabs Method Code 1E3
Aqua Regia ICPOES for the multi element and Code 1A2 Fire Assay AA for gold. Over-limit antimony
samples were analysed using Actlabs Method Code FUS-Na2O2 Special Fusion Method. Actlabs also
has standard QA/QC protocols which are reported with each assay batch.
Significant-interval c omposites in Tables 2, 3 and 4 were selected and weighted averages calculated
without upper cut-offs and below-detection limit samples, if included in a composite, were cut to 50% of the
value.
7
Table 1 – PC Pond 2026 Grab Sample Results to 25-08-26
Table 2 – PC Pond 2026 Channel Sample Mineralization Results to 25-08-26
SampleNo East8321 North8321 Elev_GPS Sample Type Prospect Area Au Ag Cu Mo Pb Pb Sb Zn Zn
g/t g/t ppm ppm ppm % ppm ppm %
C00237554 652918 5494099 grab Trench 3 Area 1.71 40.6 2080 <1 11000 1.10 94 25600 2.56
C00237555 652702 5494123 grab Trench 3 Area 0.791 17.2 4 2 4940 36 1010
C00237556 652554 5494489 grab Trench 4 Area 11.8 28.2 169 <1 6080 0.61 679 17400 1.74
C00237557 653085 5494442 grab 0.027 1.4 64 18 56 8 3850
C00237558 653082 5494444 grab 0.009 1.5 130 40 101 8 5450
C00237559 653076 5494449 grab <0.005 1 19 14 114 5 170
411487 652671 5494706 grab Trench 5 Area 2.02 5.4 198 <1 260 48 177
411488 652670 5494707 grab Trench 5 Area 0.176 6.5 25 1 5880 0.59 16 522
Sample# Trench-Channel Channel Channel Channel Interval LithoCode Au Ag Mo Pb Pb Sb Zn Zn Weighted Intercepts Channel
Designation Length (m) From (m) To (m) Length (m) gpt gpt ppm ppm % ppm ppm % Au gpt Ag gpt Mo ppm Pb % Sb ppm Zn % Length (m)
411400 TRPC26-04A-01A 0.8 0 0.57 0.57 1B 0.394 1.8 0.5 176 18 329 0.51 2.09 0.8
411401 TRPC26-04A-01A 0.8 0.57 0.8 0.23 QV 0.794 2.8 3 414 43 252
411404 TRPC26-04B-02A 0.7 0 0.7 0.7 1B 0.0025 4.6 0.5 996 94 1570
411405 TRPC26-04B-02B 1.1 0 0.45 0.45 1B/1J 1.49 84.7 0.5 16800 1.68 629 14600 1.46 1.49 84.7 1.68 629 1.46 0.45
411406 TRPC26-04B-02B 1.1 0.45 1.1 0.65 1B 0.008 0.25 0.5 43 19 180
411407 TRPC26-04B-03 2.5 0 0.52 0.52 1B 0.189 6 0.5 1100 54 2370 0.52
411408 TRPC26-04B-03 2.5 0.52 1.32 0.8 1B/1J 0.01 0.25 0.5 80 31 378
411409 TRPC26-04B-03 2.5 1.32 1.92 0.6 SZ 6.05 226 5 52100 5.21 4380 2830 6.05 226 5.21 4380 0.60
411410 TRPC26-04B-03 2.5 1.92 2.5 0.58 1B 0.031 0.6 0.5 208 48 307
411411 TRPC26-04B-04 1.7 0 0.4 0.4 4C 0.11 15.1 1 2290 0.229 31 700 0.76 46.00 1.26 1.20
411412 TRPC26-04B-04 1.7 0.4 1.2 0.8 SZ 1.57 90.2 3 17700 1.77 248 4500
411413 TRPC26-04B-04 1.7 1.2 1.7 0.5 1B 0.008 0.25 0.5 121 21 668
411443 TRPC26-02-11 1.98 1.18 1.98 0.8 4D 0.071 0.7 115 79 7 1260 114.7 1.98
411444 TRPC26-02-11 1.98 0.59 1.18 0.59 4D 0.028 0.8 51 112 8 223
411445 TRPC26-02-11 1.98 0 0.59 0.59 4D 0.008 0.25 178 21 2.5 86
411446 TRPC26-02-12 1.38 0.63 1.38 0.75 4D 0.0025 0.25 227 21 2.5 43 166.7 1.38
411447 TRPC26-02-12 1.38 0 0.63 0.63 4D 0.0025 0.25 95 14 2.5 39
411451 TRPC26-02-14 1.22 0.7 1.22 0.52 4D 0.0025 0.25 165 38 2.5 180 124.8 1.22
411452 TRPC26-02-14 1.22 0 0.7 0.7 4D 0.0025 0.25 95 18 2.5 107
411453 TRPC26-02-15 4.23 3.59 4.23 0.64 2J 0.017 0.25 34 30 2.5 247
411454 TRPC26-02-15 4.23 3.19 3.59 0.4 2J 0.007 0.25 108 45 5 235
411455 TRPC26-02-15 4.23 2.62 3.19 0.57 SZ/QV 1.21 51.3 918 7060 0.706 58 22100 2.21 1.21 51.3 918 0.706 2.21 0.57
411456 TRPC26-02-15 4.23 2.37 2.62 0.25 2J 0.04 0.25 79 194 2.5 319
411457 TRPC26-02-15 4.23 1.82 2.37 0.55 4K 0.015 0.25 83 117 2.5 267
411458 TRPC26-02-15 4.23 1.09 1.82 0.73 2J 0.0025 0.25 44 96 5 294
411460 TRPC26-02-15 4.23 0.73 1.09 0.36 SZ/QV 0.072 1.6 105 99 10 2910
411461 TRPC26-02-15 4.23 0 0.73 0.73 1A/1I 0.0025 0.25 12 12 2.5 221
411462 TRPC26-02-16 1.93 1.18 1.93 0.75 1A 0.0025 0.25 121 16 2.5 162 121 0.75
411463 TRPC26-02-16 1.93 0.5 1.18 0.68 1A 0.0025 0.25 73 16 2.5 165
411464 TRPC26-02-16 1.93 0 0.5 0.5 1A 0.0025 0.25 35 11 2.5 160
411466 TRPC26-02-18 0.39 0.23 0.39 0.16 SZ 0.166 5.3 10 257 13 11300 1.13
411467 TRPC26-02-18 0.39 0 0.23 0.23 1A 0.023 0.25 23 3 2.5 400
411468 TRPC26-02-19 1.84 1.14 1.84 0.7 1A 0.069 3.2 5 11 11 106
411469 TRPC26-02-19 1.84 0.44 1.14 0.7 1A/1J 0.023 0.9 3 375 11 421
411470 TRPC26-02-19 1.84 0 0.44 0.44 SZ/QV 0.466 14.3 70 1960 34 23000 2.3 0.466 14.3 2.3 0.44
411471 TRPC26-02-20 3.45 0 0.5 0.5 SZ/QV 2.08 129 14 30500 3.05 181 20500 2.05 2.47 51.57 1.58
411472 TRPC26-02-20 3.45 0.5 1.15 0.65 1A/1J 2.31 14.8 14 1460 51 1380
411473 TRPC26-02-20 3.45 1.15 1.58 0.43 SZ 3.16 17.1 5 1700 88 96
411474 TRPC26-02-20 3.45 1.58 2.45 0.87 2J 0.039 4.2 6 432 15 1380
411475 TRPC26-02-20 3.45 2.45 3.45 1 1I 0.012 0.25 0.5 17 6 184
411476 TRPC26-02-21 3.57 1.71 2.41 0.7 1A/1J 0.037 1.7 7 120 8 174
411477 TRPC26-02-21 3.57 0.81 1.71 0.9 1A 0.114 1.8 69 150 7 248
411478 TRPC26-02-21 3.57 0.56 0.81 0.25 SZ 0.317 6.6 67 732 13 3230
411479 TRPC26-02-21 3.57 0 0.56 0.56 1A/1J 0.053 6.6 34 1520 16 1370
411480 TRPC26-02-21 3.57 3.31 3.57 0.26 SZ 3.35 41.3 694 5770 0.577 90 3040 1.76 24.00 532.6 0.86
411481 TRPC26-02-21 3.57 2.91 3.31 0.4 1A 0.055 19.7 297 4760 42 3600
411482 TRPC26-02-21 3.57 2.71 2.91 0.2 SZ/FLT 3.12 10.1 794 1300 85 255
411483 TRPC26-02-21 3.57 2.41 2.71 0.3 1A 0.042 1.4 15 403 5 329
411484 TRPC26-02-22 1.13 0 0.48 0.48 1A 0.073 6.9 10 1030 14 879
411485 TRPC26-02-22 1.13 0.48 0.73 0.25 SZ/QV 4.02 53.2 290 15300 1.53 137 9410 0.93 16.47 69.8 1.13
411486 TRPC26-02-22 1.13 0.73 1.13 0.4 1A 0.032 0.6 4 125 7 525
8
Table 3 – PC Pond Mineralized Drill Core Mineralized Sample Results to 25-08-2026
Hole ID Sample From To Sample Au Ag Cu Cu Mo Pb Pb Sb Zn Zn Weighted Intercepts Intercept
Length (m) gpt gpt ppm % ppm ppm % ppm ppm % Au gpt Ag gpt Cu % Mo ppm Pb % Sb ppm Zn % Length (m)
PC26-03 250163 34.55 34.89 0.34 0.35 22.6 246 0.5 >5000 0.66 46 7100 0.71 0.35 22.6 0.34
PC26-03 250176 44.38 45.07 0.69 0.29 19.9 541 45 4740 26 >10000 5.52 0.29 19.9 5.52 0.69
PC26-03 250193 58.00 59.30 1.30 0.63 2.2 217 188 282 168 4340 0.63 188 1.30
PC26-03 250197 61.42 61.64 0.22 6.87 17 256 73 1640 109 5680 3.68 10.7 0.67
PC26-03 250200 61.64 62.09 0.45 2.12 7.6 153 43 359 56 487
PC26-03 250209 69.00 70.00 1.00 0.23 1.1 30 123 203 16 645 0.23 1.1 123 1.00
PC26-03 250231 86.00 86.35 0.35 0.10 0.9 47 227 52 10 1250 0.06 0.4 176.6 1.35
PC26-03 250232 86.35 87.35 1.00 0.04 0.25 26 159 30 5 285
PC26-03 250238 91.85 92.48 0.63 0.20 1.3 53 143 97 18 1120 0.30 1.8 115.3 0.83
PC26-03 250239 92.48 92.68 0.20 0.60 3.4 28 28 211 14 243
PC26-03 250246 95.97 96.35 0.38 0.33 1.6 55 110 90 18 1630 0.33 1.6 110 0.38
PC26-03 250259 105.40 106.13 0.73 0.01 0.25 25 174 7 2.5 87 174 0.73
PC26-03 250272 115.90 116.90 1.00 0.03 0.25 26 129 16 5 178 129 1.00
PC26-03 250274 117.90 118.90 1.00 0.02 0.25 37 183 28 7 212 183 1.00
PC26-03 250293 133.00 133.72 0.72 0.06 0.25 72 139 12 11 723 139 0.72
PC26-03 250296 135.15 135.94 0.79 0.22 1.3 130 145 56 30 1060 145 0.79
PC26-03 250299 137.50 138.50 1.00 0.01 0.25 29 172 10 6 3160 172 1.00
PC26-03 250306 143.00 144.00 1.00 0.02 0.25 21 417 37 2.5 300 417 1.00
PC26-03 250334 165.10 166.10 1.00 0.12 0.5 88 134 91 6 383 134 1.00
PC26-04 250363 41.37 41.66 0.29 0.26 23.9 4660 1 24 17 1870 0.26 23.9 0.29
PC26-04 410064 207.83 208.14 0.31 0.19 38.8 757 1 >5000 1.34 389 >10000 1.42 0.19 38.8 1.34 1.42 0.31
PC26-05 no significant values
PC26-06 410348 113.85 114.15 0.3 1.10 0.6 4 1 31 52 60 1.10 0.30
PC26-06 410350 114.15 115 0.85 0.08 0.25 13 2 20 41 154
PC26-06 410351 115 115.26 0.26 0.48 15.3 461 1 155 89 >10000 1.71 0.48 15.3 1.71 0.26
PC26-06 412340 174.58 175.54 0.96 0.11 24.2 3320 0.33 0.5 27 10 1040 0.23 61.2 0.78 6.22
PC26-06 412342 175.54 176.54 1.00 0.01 0.3 5 0.00 0.5 1 2.5 3
PC26-06 412343 176.54 177.54 1.00 0.20 39.3 6300 0.63 0.5 17 9 1010 Including 0.42 120.0 1.47 2.66
PC26-06 412344 177.54 177.90 0.36 0.62 118.0 >10000 1.96 0.5 22 12 1290 Including 0.56 168.5 1.97 1.66
PC26-06 410374 177.90 178.90 1.00 0.49 192 >10000 1.78 0.5 34 16 1500
PC26-06 410375 178.90 179.20 0.30 0.71 151 >10000 2.64 0.5 27 20 1530
PC26-06 410376 179.20 180.20 1.00 0.11 25.7 4340 0.43 0.5 23 15 623
PC26-06 412345 180.20 180.80 0.60 0.16 20.9 3160 0.32 0.5 30 14 560
PC26-06 410378 183.77 183.88 0.11 1.14 0.9 80 0.5 30 24 581 1.14 0.9 0.11
PC26-06 410398 209.07 209.22 0.15 0.83 10.7 1620 11 65 19 3740 0.32 13.9 1.15
PC26-06 410399 209.22 210.22 1.00 0.25 14.4 2850 0.5 13 19 436
PC26-07 410407 33.06 33.46 0.4 0.58 4.3 239 0.5 609 145 4500 0.58 4.3 0.40
PC26-07 410416 56.05 56.4 0.35 0.57 10.4 298 0.5 1320 44 >10000 1.26 1.85 12.4 1.84 0.50
PC26-07 410417 56.4 56.55 0.15 4.86 17.1 259 0.5 1240 178 >10000 3.19
PC26-08 410523 3.2 3.77 0.57 1.72 9.1 1310 0.5 117 17 >10000 1.14 1.72 9.1 1.14 0.57
PC26-08 410527 5.84 6.43 0.59 0.90 9.3 530 1 119 79 1110 0.90 9.3 0.59
PC26-08 410542 13.47 14.25 0.78 0.19 11.8 1730 1 24 21 >10000 3.93 0.19 11.8 3.93 0.78
PC26-08 410554 33.25 33.52 0.27 0.51 0.25 49 3 51 14 449 0.51 0.27
PC26-08 410562 41.6 41.8 0.2 1.33 7.5 554 0.5 853 313 >10000 5.53 0.96 5.7 3.79 0.41
PC26-08 410565 41.8 42.01 0.21 0.62 4 586 0.5 390 134 >10000 2.13
PC26-08 410569 47 47.64 0.64 0.07 12.3 632 1 327 12 >10000 5.13 0.07 12.3 5.13 0.64
PC26-08 410572 48 48.41 0.41 0.46 12.1 2030 96 359 109 >10000 2.71 0.34 8.6 1.80 1.20
PC26-08 410573 48.41 48.8 0.39 0.42 6.7 621 7 171 167 >10000 1.18
PC26-08 410576 48.8 49.2 0.4 0.13 6.9 602 13 123 30 >10000 1.48
PC26-08 410577 49.2 50.2 1 0.04 1.2 250 118 103 13 1870 118 1.00
PC26-08 410579 51.1 52.07 0.97 0.09 15.4 2000 3 53 10 3320 15.4 0.97
PC26-08 410584 53.5 53.65 0.15 1.34 2.9 5 8 80 52 280 1.34 2.9 0.15
PC26-08 410609 73.56 73.85 0.29 0.27 16.7 3200 0.5 24 17 2270 0.71 7.3 0.76
PC26-08 410610 73.85 74.08 0.23 0.73 1.1 21 3 27 44 86
PC26-08 410613 74.08 74.32 0.24 1.21 1.9 37 4 44 53 451
PC26-08 410629 85.9 86.9 1 0.10 18.8 3910 1 11 14 433 0.14 24.9 2.44
PC26-08 410631 86.9 87.67 0.77 0.17 26.3 5780 0.5 13 9 489
PC26-08 410632 87.67 88.34 0.67 0.17 32.3 6660 0.5 19 2.5 1080
PC26-08 410713 175 175.72 0.72 0.94 4.8 1270 0.5 6 10 253 0.94 4.8 0.72
PC26-09 no significant values
PC26-10 410759 10.90 11.19 0.29 2.11 1.7 163 0.5 149 19 1560 2.11 1.7 0.29
PC26-10 410856 180.38 180.92 0.54 0.49 19.0 15 0.5 >5000 0.574 149 4220 0.47 14.2 1.41
PC26-10 410857 180.92 181.26 0.34 0.62 11.6 8 4 3590 387 904
PC26-10 410860 181.26 181.79 0.53 0.35 10.9 32 0.5 2480 132 7160
PC26-11 410908 78.8 78.95 0.15 1.13 2.1 98 0.5 145 43 1930 1.13 2.1 0.15
PC26-11 410924 98.47 98.69 0.22 1.14 0.25 235 1 14 55 69 1.14 0.3 0.22
PC26-11 410932 110.66 111.47 0.81 0.57 0.25 65 0.5 28 18 138 0.57 0.3 0.81
PC26-12 410969 3.45 4.45 1.00 0.22 0.9 35 3 11 6 109 0.64 2.0 2.64
PC26-12 410970 4.45 5.45 1.00 0.84 2.2 29 2 27 36 34
PC26-12 410971 5.45 6.09 0.64 1.00 3.5 156 6 45 50 30
PC26-12 412036 115.49 115.59 0.10 1.06 0.3 19 0.5 17 30 67 1.06 0.3 0.10
PC26-13 412088 96.15 97.09 0.94 0.61 15.9 73 3 >5000 0.51 537 1620 0.61 15.9 0.51 537 0.94
PC26-13 412095 100.96 101.80 0.84 0.10 12.9 757 0.5 789 100 332 0.25 18.5 1.64
PC26-13 412096 101.80 102.60 0.80 0.41 24.4 2160 2 706 137 404
PC26-13 412102 107.28 108.12 0.84 0.45 22.6 59 3 3470 66 6500 0.65 0.45 22.6 0.65 0.84
PC26-14 412133 32.68 33.00 0.32 0.50 20.6 93 0.5 4300 0.43 48 4410 0.44 0.39 19.2 0.40 0.56 2.32
PC26-14 412134 33.00 33.17 0.17 2.58 129.0 414 1 >5000 2.28 399 >10000 4.63 Including 1.22 58.2 1.07 1.89 0.49
PC26-14 412137 33.17 33.75 0.58 0.11 2.3 24 0.5 434 0.04 23 827 0.08
PC26-14 412138 33.75 34.50 0.75 0.14 9.8 43 3 2340 0.23 31 1800 0.18
PC26-14 412139 34.50 35.00 0.50 0.29 14.7 54 3 3930 0.39 35 3680 0.37
PC26-14 412187 117.95 118.42 0.47 0.39 14.7 454 22 1760 86 4540 0.39 14.7 0.47
PC26-15 412208 5.60 6.60 1.00 0.51 0.9 74 2 96 13 271 0.51 1.00
PC26-15 412298 270.66 271.66 1.00 0.17 0.3 43 0.5 6 28 717
PC26-15 412299 271.66 272.62 0.96 0.45 0.3 19 1 6 37 117 0.58 1.1 1.26
PC26-15 412302 272.62 272.92 0.30 0.99 3.8 238 0.5 497 60 5470
PC26-16 412307 8.36 8.55 0.19 0.22 0.8 101 10900 635 17 536 0.10 0.8 2097 1.64
PC26-16 412310 8.55 9.55 1.00 0.09 1.0 802 58 7 10 149
PC26-16 412311 9.55 10.00 0.45 0.06 0.3 305 2910 38 10 121
PC26-16 412327 43.22 43.95 0.73 0.25 7.6 4080 67 29 13 269 0.23 3.7 70 2.02
PC26-16 412328 43.95 44.95 1.00 0.02 1.4 530 26 19 8 122
PC26-16 412329 44.95 45.24 0.29 0.96 2.0 77 230 622 65 1020
PC26-16 412356 58.20 58.42 0.22 0.04 30.5 283 10 >5000 0.61 18 2480 0.51 43.8 20 1.19 0.39
PC26-16 412357 58.42 58.59 0.17 1.13 61.1 774 5 >5000 1.95 48 9770
PC26-16 412371 65.94 66.94 1.00 0.98 0.3 24 25 4 2.5 62 0.46 11.4 3.15
PC26-16 412372 66.94 67.94 1.00 0.01 0.3 11 16 17 7 93
PC26-16 412373 67.94 68.83 0.89 0.01 0.5 13 87 72 8 361
PC26-16 412374 68.83 69.09 0.26 1.67 135.0 889 787 >5000 1.10 453 >10000 2.28 Including 1.67 135.0 787 1.10 453 2.28 0.26
PC26-16 412416 100.36 101.47 1.11 0.61 10.0 92 973 2400 40 2970 0.61 10.0 973 1.11
PC26-16 412425 105.20 105.60 0.40 0.34 5.3 123 979 814 96 4220 0.34 5.3 979 0.40
PC26-16 412432 110.10 110.70 0.60 0.38 7.0 64 509 781 118 2430 0.19 3.8 352 1.90
PC26-16 412435 110.70 111.67 0.97 0.04 1.7 59 231 159 65 1290
PC26-16 412436 111.67 112.00 0.33 0.29 4.4 54 425 448 88 2400