ARRAS MINERALS EXPANDS THE BEREZSKI TREND (ELEMES PROJECT) & PROVIDES 2025 YEAR END EXPLORATION UPDATE
TSX-V: ARK / OTCQB: ARRKF
Highlights include:
- KGK drilling successfully expanded the Berezski East footprint to >1,000 m of strike length
- Northern and southern extensions of the Berezski Central target identified
- Multiple new Cu-Au mineralized zones discovered between known targets
- Drill hole NOV25003 intersected porphyry-style mineralization 1.6 km southwest of Berezski Central, indicating a >2 km southern extension of the Berezski Trend under cover
- Gravity data shows strong correlation between mineralization and gravity lows
Top of Bedrock (KGK) Drilling at Berezski Central and Berezski East
Preliminary data from the Berezski gravity survey identified that the Berezski Central and Berezski East targets may be part of much larger system. However, the minimal outcrop exposure in the area has made geological mapping challenging, and in October, a 64-hole top-of-bedrock (KGK) drill program, totaling 1,663 m was completed over these targets.
The program was designed to rapidly evaluate the geology and mineralization found beneath shallow cover in this area, and to evaluate if KGK drilling would be a useful technique to rapidly evaluate the 8.8 km-long Berezski Trend to see if it hosts additional Cu-Au zones.
|
KGK hole ID |
Intersection |
Interval |
Au |
Cu |
Ag |
Mo |
|
|
From (m) |
To (m) |
(m) |
(g/t) |
( %) |
(g/t) |
(ppm) |
|
|
ELKGK25004 |
5.00 |
13.00 |
8.00 |
0.14 |
0.00 |
1.43 |
2.75 |
|
ELKGK25005 |
0.00 |
29.00 |
29.00 |
0.83 |
0.49 |
1.71 |
141.34 |
|
ELKGK25006 |
13.00 |
19.00 |
6.00 |
0.04 |
0.21 |
0.80 |
163.00 |
|
ELKGK25009 |
27.00 |
29.00 |
2.00 |
0.15 |
0.00 |
2.50 |
2.00 |
|
ELKGK25011 |
0.00 |
28.00 |
28.00 |
0.11 |
0.04 |
0.50 |
2.04 |
|
ELKGK25013 |
7.00 |
15.00 |
8.00 |
0.23 |
0.02 |
0.50 |
4.25 |
|
And |
39.00 |
45.00 |
6.00 |
0.14 |
0.01 |
0.50 |
2.00 |
|
ELKGK25020 |
5.00 |
7.00 |
2.00 |
0.12 |
0.01 |
0.50 |
1.00 |
|
ELKGK25021 |
0.00 |
37.00 |
37.00 |
0.15 |
0.09 |
1.21 |
66.16 |
|
ELKGK25027 |
7.00 |
22.00 |
15.00 |
0.68 |
0.09 |
0.00 |
1.93 |
|
ELKGK25028 |
11.00 |
47.00 |
36.00 |
0.13 |
0.01 |
0.75 |
2.33 |
|
ELKGK25029 |
19.00 |
23.00 |
4.00 |
0.61 |
0.02 |
0.60 |
3.00 |
|
ELKGK25030 |
0.00 |
20.00 |
20.00 |
0.19 |
0.01 |
0.00 |
1.85 |
|
ELKGK25037 |
3.00 |
7.00 |
4.00 |
0.32 |
0.02 |
1.40 |
45.00 |
|
ELKGK25043 |
0.00 |
24.00 |
24.00 |
2.00 |
0.21 |
0.51 |
1.83 |
|
ELKGK25044 |
15.00 |
17.00 |
2.00 |
0.31 |
0.01 |
0.50 |
4.00 |
|
ELKGK25054 |
23.00 |
33.00 |
10.00 |
0.15 |
0.16 |
2.00 |
57.60 |
|
And |
75.00 |
89.00 |
14.00 |
0.13 |
0.05 |
1.13 |
26.86 |
|
ELKGK25059 |
0.00 |
21.00 |
21.00 |
0.21 |
0.01 |
0.60 |
1.76 |
|
And |
33.00 |
41.00 |
8.00 |
2.52 |
0.01 |
2.18 |
3.00 |
|
ELKGK25060 |
0.00 |
23.00 |
23.00 |
0.20 |
0.01 |
0.62 |
13.90 |
|
ELKGK25061 |
7.00 |
8.00 |
1.00 |
0.15 |
0.01 |
1.10 |
1.00 |
The KGK drilling program delivered strong results, materially expanding the copper-gold mineralized footprint at the Berezski Central and Berezski East targets to over 1000 m of strike length and indicated that the mineralization was still open to the north and south.
The KGK drilling also identified several previously unknown zones of gold mineralization between the Berezski Central and Berezski East, demonstrating potential beyond the known target areas as shown in Figure 2.
Novii Target
Three holes, totaling 922.2 m, were completed at
Hole NOV25001: This hole was drilled 4.3 km to the southwest of the Berezski Central target. The hole Intersected a thick package of andesites and volcaniclastics with several narrow breccia zones, and with weak alteration and minor disseminated pyrite.
Hole NOV25002: This hole was drilled 6.4 km to the southwest of the Berezski Central target. The hole intersected a thick sequence of sediments, interbedded siltstones and limestones, before passing into a sequence of lithic tuffs with weak alteration and minor pyrite.
Hole NOV25003: This hole is located approximately 1,600 m southwest of Berezski Central. The hole was collared in weakly propylitic altered volcano-sedimentary rocks to 190 m depth, where the hole passed into argillic altered diorites, with local relict K-Feldspar and quartz alteration. The diorites were cut by several breccia zones, that included fragments of B-type veins. Mineralization is dominated by disseminated pyrite with minor chalcopyrite starting from 100 m depth and continuing to the end of the drill-hole.
The Company believes that this discovery of porphyry-style mineralization in NOV25003, 1.6 km to the southwest of Berezski Central, suggests it has intersected the margin of a previously unrecognized porphyry system, which is strongly supported by the ground magnetic survey data. This hole is also located on the eastern edge of the gravity low anomaly. The new data from NOV25003 supports the theory that the Berezski Trend is much larger than originally thought and supports the idea that there is a thin cover unit masking the southern extension of the 8.8 km long copper-in-coil anomaly to the south of Berezski Central. Further drill testing of the
|
Table 2. Summary results from holes NOV25003 |
|||||||||
|
Hole_ID |
Intersection |
Interval |
Au |
Cu |
Ag |
Mo |
CuEq |
AuEq |
|
|
|
From (m) |
To (m) |
(m) |
(g/t) |
( %) |
(g/t) |
ppm |
( %) |
(g/t) |
|
NOV25003 |
223.90 |
236.00 |
12.10 |
0.12 |
0.06 |
0.61 |
20.16 |
0.19 |
0.16 |
|
& |
249.00 |
306.00 |
57.00 |
0.10 |
0.07 |
0.37 |
26.40 |
0.18 |
0.15 |
|
that includes |
249.00 |
263.00 |
14.00 |
0.23 |
0.08 |
0.45 |
21.31 |
0.32 |
0.27 |
|
& |
326.00 |
368.70 |
42.70 |
0.08 |
0.07 |
0.62 |
18.10 |
0.16 |
0.13 |
|
including |
326.00 |
352.00 |
26.00 |
0.09 |
0.08 |
0.72 |
22.60 |
0.18 |
0.16 |
|
that includes |
364.00 |
368.70 |
4.70 |
0.10 |
0.09 |
0.79 |
21.99 |
0.20 |
0.17 |
|
Notes: For copper and gold equivalent calculations the following metal process were used: |
2025 Year End Exploration Update
The Company commenced field work at Elemes in April following the successful completion of a
Berezski Trend:
The 8.8 km Berezski Trend located within the
2025 Exploration Summary Highlights:
- Completed a 64.9 sq km Vector Induced Polarization survey over the Aimandai Trend
- Completed a 24.6 line-km Pole-Dipole Induced Polarization survey at Aimandai exploration targets
- Completed 26 holes totaling approximately 10,000 m of core drilling on the Berezski Trend.
- Completed a 64 hole, 1,663 m top of bedrock (KGK) drill program over the Berezski Central/Berezski East target areas.
- Completed 75 sq km Magnetotellurics (MT and Gravity surveys over the high-priority areas of the Berezski and Aimandai trends
Geophysics: Preliminary results from the gravity survey have been very encouraging. The gravity survey identified several broad gravity lows that appear to be associated with the mineralization intersected at Berezski Central and Berezski East and may appear to be mapping out the large alteration footprints of these systems. Encouragingly, the survey identified several untested gravity lows that could suggest additional porphyry-hydrothermal systems along the Berezski Trend. While early, we believe this to be potentially an important new vector we can follow to further targets to be drilled in 2026.
The high pyrite content observed in the drill core from the Berezski drilling suggests that the effectiveness of IP surveys at the Berezski Trend may be limited. The Company believed that an MT survey may be more effective on identifying anomalies under cover and at depth, and as a result, the Company completed a 75 sq km MT survey. The data collection for this survey was completed in
Top of Bedrock Drilling (KGK): A 64-hole top-of-bedrock (KGK) drill program, totaling 1,663 m, was completed over these targets. Results from this program are discussed earlier in this press release.
Drilling commenced in
Selected intercepts from the Berezski Central Target:
|
Hole ID |
Intersection |
Interval |
Au |
Cu |
Ag |
Mo |
CuEq |
AuEq |
|
|
|
From (m) |
To (m) |
(m) |
(g/t) |
( %) |
(g/t) |
ppm |
( %) |
(g/t) |
|
EL24001 |
0.0 |
476.5 |
476.50 |
0.25 |
0.17 |
0.70 |
57.00 |
0.38 |
0.44 |
|
Including |
22.0 |
283.0 |
261.00 |
0.39 |
0.24 |
1.00 |
75.00 |
0.57 |
0.66 |
|
EL24002 |
2.0 |
188.0 |
186.00 |
0.30 |
0.09 |
0.60 |
29.00 |
0.35 |
0.40 |
|
Including |
2.0 |
36.0 |
34.00 |
0.38 |
0.16 |
1.00 |
80.00 |
0.50 |
0.58 |
|
EL24003 |
41.0 |
305.0 |
264.00 |
0.17 |
0.09 |
0.40 |
44.00 |
0.24 |
0.28 |
|
EL24011 |
247.0 |
323.0 |
76.00 |
0.14 |
0.06 |
0.90 |
8.00 |
0.18 |
0.21 |
|
EL25012 |
3.0 |
581.0 |
578.00 |
0.21 |
0.14 |
0.49 |
42.14 |
0.31 |
0.37 |
|
Including |
137.0 |
577.0 |
440.00 |
0.25 |
0.16 |
0.55 |
42.64 |
0.36 |
0.42 |
|
EL25018 |
52.0 |
244.0 |
192.00 |
0.19 |
0.13 |
0.79 |
62.40 |
0.30 |
0.35 |
|
Including |
52.0 |
156.0 |
104.00 |
0.25 |
0.16 |
0.96 |
96.10 |
0.40 |
0.46 |
|
EL25020 |
358.1 |
672.0 |
313.90 |
0.14 |
0.12 |
0.43 |
48.40 |
0.24 |
0.28 |
|
Including |
475.0 |
604.0 |
129.00 |
0.16 |
0.16 |
0.48 |
58.20 |
0.30 |
0.34 |
|
Notes: For copper and gold equivalent calculations the following metal process were used: |
|
Hole ID |
Intersection |
Interval |
Au |
Cu |
Ag |
Mo |
CuEq |
AuEq |
|
|
|
From (m) |
To (m) |
(m) |
(g/t) |
( %) |
(g/t) |
ppm |
( %) |
(g/t) |
|
EL24004 |
1.2 |
306.0 |
304.80 |
0.46 |
0.07 |
0.40 |
3.00 |
0.45 |
0.53 |
|
Including |
1.2 |
196.0 |
194.80 |
0.59 |
0.08 |
0.40 |
3.00 |
0.57 |
0.66 |
|
EL25019 |
0.0 |
457.5 |
457.50 |
0.61 |
0.10 |
0.48 |
2.69 |
0.60 |
0.70 |
|
Includes |
0.0 |
231.0 |
231.00 |
0.97 |
0.13 |
0.53 |
2.19 |
0.93 |
1.09 |
|
Notes: For copper and gold equivalent calculations the following metal process were used: |
|
Hole ID |
Intersection |
Interval |
Au |
Cu |
Ag |
Mo |
CuEq |
AuEq |
|
|
|
From (m) |
To (m) |
(m) |
(g/t) |
( %) |
(g/t) |
ppm |
( %) |
(g/t) |
|
EL24005 |
14.0 |
561.0 |
547.00 |
0.48 |
0.23 |
2.30 |
25.30 |
0.62 |
0.72 |
|
Including |
24.0 |
230.0 |
206.00 |
0.54 |
0.27 |
4.80 |
29.70 |
0.73 |
0.85 |
|
EL24006 |
4.0 |
60.0 |
56.00 |
0.33 |
0.36 |
1.20 |
3.80 |
0.57 |
0.67 |
|
EL24010 |
262.0 |
414.0 |
152.00 |
0.06 |
0.07 |
0.30 |
3.20 |
0.11 |
0.13 |
|
EL25014A |
130.0 |
284.0 |
154.00 |
0.72 |
0.29 |
3.43 |
53.50 |
0.90 |
1.04 |
|
EL25016 |
0.0 |
276.0 |
276.00 |
0.32 |
0.21 |
3.70 |
2.00 |
0.47 |
0.55 |
|
Including |
0.0 |
158.0 |
158.00 |
0.48 |
0.33 |
6.00 |
2.80 |
0.72 |
0.84 |
|
Notes: For copper and gold equivalent calculations the following metal process were used: |
Berezski Central Results: Drilling continues to expand the footprint of the porphyry Cu-Au mineralization to approximately 600 m x 500 m. Drilling has also confirmed that mineralization extends to at least 600 m depth, showing that there is a robust porphyry system at this target.
Berezski East Results: Drillhole EL25019 delivered an exceptional high-grade gold-copper intercept from surface at Berezski East. The hole intersected broad zones of potassic alteration and the presence of copper minerals such as bornite and chalcopyrite suggests this target, originally thought to be related to an epithermal system, may form part of a larger porphyry system. The KGK drilling appears to have expanded the footprint of the Berezski East mineralization to at least a 1000 m strike length, a highly encouraging development.
Berezski North Results: Drilling at Berezski North continues to demonstrate the presence of a large porphyry system at Berezski North. Drilling has defined a 600 m NW-SE trending zone at Berezski North that remains open in the northwest and southeast directions and at depth. Hole EL25016, approximately 300 m southeast of Hole EL24005 intersected thick zones of high-grade copper-gold mineralization from surface, and drill-holes EL25014A and EL25027 (results pending) intersected thick zones of high-grade mineralized breccias in the former, and zones of porphyry-style mineralization in the latter, demonstrating that we're vectoring towards the core of the system.
Drilling & Assays Pending: The drilling program will pause for approximately six weeks over the holiday period with the drill rigs undergoing planned maintenance and are expected to restart in February. Assay turnarounds incurred a four-week export delay to the ALS analytical lab in
Aimandai Trend: A Vector IP and IP survey was conducted over the Aimandai Trend, a 14 km copper-in-soil anomaly located approximately 7 km east of the Berezski Trend. This was followed by an 18.5-square km MT and Gravity survey targeting priority areas of the Trend. Data analysis and final results are expected by year-end and the Company will be evaluating and ranking exploration targets at this target area in the New Year.
Stepnoe & Ekidos Projects
The Stepnoe and Ekidos licenses cover early Ordovician aged rocks of the lower Boshchekul-Chingiz volcanic arc that hosts the Beskauga Deposit. The licenses are covered by a 10-50m thick cover sequence of soil and lacustrine sediments. The Company completed a large top of bedrock (KGK) drill program (659 holes totaling 20,099 meters) in
The KGK drilling showed that the geology of the Stepnoe-Ekidos area is mostly composed of fine-grained weakly magnetic tuffs, highly magnetic crystal tuffs, lithic tuffs and andesites. Sedimentary rocks are present, dominated by siltstones. The drilling also identified multiple dioritic intrusions cutting through this andesite-volcano-sedimentary sequences.
The assay results from the final 22 holes are still pending. However, the Company believes that the drilling has identified path-finder geochemistry and alteration signatures related to 2-3 discrete porphyry systems in the license areas.
Ekidos Central: A nearly 2 km long Northwest-Southeast trending Copper KGK anomaly associated with diorites stocks emplaced into tuffs, with associated argillic and propylitic alteration.
Ekidos South: A discrete >2000ppm KGK anomaly, with associated Mo, Au, Bi, Te anomaly. Assays from infill holes around this area are pending, so exact scale of the anomaly is currently unknown. Geochemical anomaly appears to be related to a silicified diorite.
Ekidos North: Approximately 1km long Northeast-Southwest trending Au-As KGK anomaly associated with a series of diorite stocks emplaced into tuffs with associated argillic alteration (Dickite) and both inner and outer Propylitic alteration (Chlorite and Epidote), that may be associated with an epithermal system.
The results from the KGK program were very encouraging, identifying potentially two porphyry systems and maybe a third, epithermal system. The Company is planning to conduct follow-up induced polarization surveys over these principal targets, with plans to drill test them in 2026.
2026 Exploration Plan
The Company is awaiting final analysis of the MT geophysical survey data along with additional drill hole assays and expects to provide an overview of the 2026 Exploration Plan in advance of recommencing drill activities in early
Elemes Project Overview:
Situated within the prolific Bozshakol-Chingiz metallogenic belt, Elemes lies near significant regional deposits, including the Beskauga porphyry copper-gold-silver deposit (approx. ~80 km east) and
Geologically, the property is underlain by interbedded intermediate volcanic and sedimentary rocks intruded by multiple phases of diorite and monzodiorite porphyry. Copper-gold mineralization occurs in sheeted and stockwork quartz-chalcopyrite veins associated with these intrusions. In addition, high-grade low-sulphidation epithermal veins have been mapped on the property, representing a secondary exploration target.
Property-wide soil sampling programs in 2022 and 2023 defined two extensive Cu-Mo-As geochemical anomalies: the Berezski and Aimandai Trends, both considered priority targets for follow-up exploration drilling. A Phase 1 drill program on the Berezski Trend in late 2024 returned high-grade porphyry/epithermal copper and gold mineralization in results announced in Q1 2025. A 20,000 m Phase 2 drill program commenced in
References
1Bozshakol Q1, 2025 Report
https://www.kazminerals.com/media/23282/q1-2025-production-report_final.pdf
Quality Assurance and Quality Control
The Company adheres to CIM Best Practices Guidelines for exploration related activities conducted on its property. Quality Assurance and Quality Control (QA/QC) procedures are overseen by the Qualified Person.
Arras Minerals QA/QC protocols are maintained through the insertion of certified reference material (standards), blanks and field duplicates within the sample stream. Drill core is cut at
Each bagged core sample was shipped to
Gold analysis was conducted by
ALS is an accredited laboratory which is independent of the Company. Chain of custody is maintained from the drill to the submittal into the laboratory preparation facility.
Qualified Person: The scientific and technical disclosure for this news release has been prepared under supervision of and approved by
Gold, copper and other mineral equivalents are calculated on the basis specifically set forth in respect thereto in this presentation and are based upon the reasonable assumptions as to the prices of various metals and their recoveries thereof made by management of the Company on a project-by-project basis as converted metal. All drill-hole intervals are reported as drill widths, as true thicknesses are unknown. Assumed metal prices are:
The Company has updated metal recoveries: 90% for copper, 85% for gold, 75% for silver, and 80% for molybdenum. These figures are based on a review of published data from advanced-stage porphyry projects (including Vizcachitas, Los Andes Copper;
Copper Equivalent ("CuEq") grades reported for the drill holes at Elemes were calculated using the following formula: CuEq % = ((Copper (%))*0.9) + ((Gold (g/t) x 0.8571)*0.85) + ((Silver (g/t) x 0.0117)*0.75) + ((Molybdenum (ppm) x 6.8568)*0.80).
Gold Equivalent ("AuEq") grades reported for the drill holes at Elemes were calculated using the following formula: AuEq g/t = ((Gold (g/t)*0.85) + ((Copper (%) x 1.1667)*0.9) + ((Silver (g/t) x 0.0136)*0.75) + ((Molybdenum (ppm) x 8.0)*0.80).
On behalf of the Board of Directors,
"Tim Barry"
Tim Barry, MAusIMM CP(Geo)
Chief Executive Officer and Director
Further information can be found on:
- the Company's website https://www.arrasminerals.com or
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About
Cautionary note regarding forward-looking statements: This news release contains forward-looking statements regarding future events and Arras' future results that are subject to the safe harbors created under the
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