Arras Minerals Corp. (TSX.V: ARK)
(“Arras”, or the “Company”) is pleased to announce assay results
from holes Bg22014, Bg22015, & Bg22017 from the ongoing drill
program at the Beskauga copper-gold deposit and surrounding area
(“Beskauga” or the “Project”).
Highlights Include:
-
Bg22015: 778.2m of mineralization grading 0.40%
copper-equivalent (“CuEq”) (0.31 g/t gold (“Au”), 0.13 %
copper (“Cu”), 0.94 g/t silver (“Ag”) starting at 40.8m.
-
Including: 95.2 m grading 0.61 % CuEq (0.47 g/t
Au, 0.20% Cu, 1.27 g/t Ag) starting at 268.0m depth down-hole.
-
Including: 322.4 m grading 0.51 % CuEq (0.40 g/t
Au, 0.16% Cu, 1.15 g/t Ag) from 446.0m depth down-hole.
-
Bg22014: 335.6m of mineralization grading 0.24 grams per
ton (“g/t”) gold-equivalent (“AuEq”) (0.16 g/t Au, 0.05 %
Cu, 0.39 g/t Ag, starting at 44.0 m to the end of the drill hole.
-
Including: 7.0 m grading 1.57g/t AuEq (1.47 g/t
Au, 0.06% Cu, 1.75 g/t Ag) starting at 44.0m depth down-hole.
-
Including: 8.0 m grading 1.14g/t AuEq (0.56 g/t
Au, 0.45% Cu, 1.12 g/t Ag) starting at 369.0 m depth
down-hole.
-
Bg22017: 499.8m of mineralization grading 0.22g/t
AuEq (0.15 g/t Au, 0.05% Cu, 0.45 g/t Ag) starting at 32.5
m to the end of the drill hole.
-
Including: 12.0 m grading 1.65g/t AuEq (1.27 g/t
Au, 0.21% Cu, 3.28 g/t Ag and 204.63 ppm Mo) starting at 376.0m
depth down-hole.
-
Including: 7.7 m grading 1.14g/t AuEq (0.94 g/t
Au, 0.09% Cu, 2.34 g/t Ag and 165.28 ppm Mo) starting at 465.3m
depth down-hole.
-
Consistent mineralization was seen for the entire length of hole
Bg22015 (1,109.8m) and further defines a high-grade core to the
Beskauga deposit within a lower grade halo.
-
Holes Bg22014 & Bg22017 were drilled 3.2km to the south of the
main Beskauga deposit and show widespread low-grade gold and copper
mineralization and suggest another mineralizing system close-by.
Very high molybdenum results were intercepted towards the bottom of
hole Bg22017.
Tim Barry, CEO of Arras, commenting on these
latest results stated, “Our drilling on the Beskauga Project has
continued to produce long intercepts of continuous copper-gold
mineralization starting at a depth of 40 meters below the surface.
Our recent drilling has demonstrated the continuity of the
mineralization to over one kilometer of vertical depth and has
defined a high-grade zone that dips to the SSW. Mineralization
remains open both laterally and at depth and suggests that the
Beskauga ore body is much larger than has been recognized in the
NI43-101 report.”
Mr. Barry continued, “Apart from the Beskauga
deposit, Arras has begun exploration on the Beskauga South area,
located about 3.2 kilometers to the south of the main deposit.
Although the mineralizing system at Beskauga South is not yet well
understood, the presence of broad zones of low-grade gold
mineralization punctuated by high-grade zones suggests there is
potential for a bulk mineable target.”
A summary of the results announced in this news
release is outlined in the table below.
Table 1. Summary table for drill holes
Bg22014, Bg22015 and Bg22017
Notes: Copper Equivalent (“CuEq”) grades reported
for the drill holes at Beskauga were calculated using the following
formula: CuEq % = Copper (%) + (Gold (g/t) x 0.8264) + (Silver
(g/t) x 0.0107) + (Molybdenum (ppm) x 3.3333). Gold Equivalent
(“AuEq”) grades reported for the drill holes at Beskauga were
calculated using the following formula: AuEq g/t = Gold (g/t) +
(Copper (%) x 1.2100) + (Silver (g/t) x 0.0129) + (Molybdenum (ppm)
x 4.0334). Assumptions used for the copper and gold equivalent
calculations were metal prices of US$3.00/lb. Copper, US$1,700/oz
Gold, US$22/oz Silver, US$10/lb. Molybdenum, and metallurgical
recoveries were assumed to be 100%.
Results of Bg22014, Bg22015 and
Bg22017:
Bg22014: was drilled just north
of the Beskauga South target, located approximately 3.2 kilometers
south of the Beskauga Main deposit. The aim of the drill hole was
to test the major NE-SW trending structure that links Beskauga
South to Beskauga Main and to test for the first time a large IP
anomaly along this part of the structure that coincides with strong
Au-Cu-Bi anomalies identified in KGK drilling.
The drill hole intersected andesite basalts and
tuffs cut by multiple intrusions of porphyritic quartz monzonite.
The andesite basalts are weakly propylitic altered (chlorite,
smectite, magnetite, and epidote), while the porphyritic quartz
monzonite shows weak potassic alteration (K-feldspar, magnetite,
epidote, and rarely biotite). The best mineralized intercepts are
hosted in the porphyritic quartz monzonite intrusions and are
related to weak quartz-pyrite veining with occasional zones of
chalcopyrite magnetite. The same style of veining can be seen
sporadically in andesite basalts but with much weaker
intensity.
Bg22015: was collared 90.0 m to
the NW from Arras drill hole Bg21006 (689.2m @ 0.76 % CuEq,
including 120.9m @ 2.35% CuEq), and drilled at angle of 85 degrees
toward the northeast with final depth of 1,109.8m. The purpose of
the hole was to test a deep Audio-magentotelluric “AMT” anomaly
which started at a depth from 725m It also aimed to further test
mineralization intersected at 595m in depth by drill hole Bg21002
(431m @ 0.68% CuEq).
The drill hole started in moderately, to very
strong, argillic altered diorite. The argillic alteration consists
of intense illite-smectite with local kaolinite, before
transitioning to very weak illite-smectite alteration. Preserved
remnants of sodic (albite-hematite) alteration starting appeared
below depth of 675.0m. Diorite is cut by three post mineral
argillic altered dykes of porphyritic diorite with average
thickness of 35.0m at depths of 363.0m, 420.0m and 620.0m and
lastly with 22.0m thick barren basalt dyke at 768.4m depth.
Mineralization occurs as quartz-tennantite-chalcopyrite-pyrite
stockwork, and sheeted veining followed by tennantite stringers and
weak dissemination of copper sulphides close around the veins. The
presence of bornite is scarce while molybdenite is found in quartz
veins beyond depth of 841.0 m.
Bg22017: was collared in fence
450m to the east from hole Bg22014, to test a magnetic anomaly
supported by anomalous gold up to 6 g/t in historical KGK drill
holes. After 32.5m of overburden the drill hole intersected a small
interval of porphyritic quartz monzonite before continuing through
andesite basalts and their associated tuffs. From 109.0m the quartz
monzonite continued to the end of drill hole, interspersed with
several small intervals of andesite basalt between depths of 301.0m
and 331.0m. Andesite basalts are weakly propylitic (chlorite,
smectite, magnetite) altered while quartz monzonite is altered by
weak potassic (K-feldspar, magnetite and rare biotite) alteration.
Mineralization is related with quartz-pyrite veining that has weak
presence of chalcopyrite and rarely magnetite.
Figure 1. Location of the holes completed
to date as part of Arras’ planned 30,000-metre drill program on the
Beskauga Main deposit and wider area. The surface projection of the
block model from the current NI-43-101 Mineral Resource Estimate is
shown for copper. The inset map in Figure 2 below shows the
location of Beskauga Main relative to Beskauga South.
Figure 2. Location of the holes completed
to date at the Beskauga South area, located approximately 3.2
kilometres SSW from the Beskauga Main deposit, and outside of the
current NI-43-101 Mineral Resource Estimate. The inset map shows
the location of Beskauga South relative to Beskauga
Main.
Figure 3. Cross-section showing drill
holes Bg22015 in relation to historical drill hole Bg-094.
Also shown are grade contours based on the Beskauga block model for
copper (only) developed for the purposes of the current Mineral
Resource Estimate for Beskauga (for further details, please see
Arras’ press release on June 20, 2022). CuEq grades of key
intercepts in Bg22015 and historical holes are shown. The
cross-section demonstrates the steep dipping high-grade
copper-gold-silver trend observed through Arras’ exploration to
date. This trend is observed beginning at the paleo-bedrock surface
(41 m in depth) and averages between 200-300 m wide and to be
consistently mineralized down to at least 1000 meters.
Figure 4. Cross-section showing
drill holes Bg22014 and Bg22017 with generalized interpretation of
intersected rock units. Key intercepts of AuEq grades in Bg22014,
Bg22017 are shown.
About the Beskauga Deposit: The
Beskauga deposit is a gold-copper-silver deposit with an
“Indicated” Mineral Resource of 111.2 million tonnes grading 0.49
g/t gold, 0.30% copper, and 1.3 g/t silver for 1.75 million ounces
of contained gold, 333.6 thousand tonnes of contained copper, and
4.79 million ounces of contained silver and an “Inferred” Mineral
Resource of 92.6 million tonnes grading 0.50 g/t gold, 0.24% copper
and 1.1 g/t silver for 1.49 million ounces of contained gold, 222.2
thousand tonnes of contained copper, and 3.39 million ounces of
contained silver. The constraining open pit was optimized and
calculated using a Gross Metal Value (“GMV”) cut-off of $20/tonne
based on a price of $1,750/oz for gold, $3.50/lb for copper, $22/oz
for silver, and with an average recovery of 85% for copper and
74.5% for gold and 50.0% for silver.
Assay and QAQC Procedures: The
drill core is cut in half lengthwise with one half (same half,
consistently) collected for analysis, and one half preserved as a
record. Bagged samples are sealed to ensure integrity during
transport.
All sample preparation and geochemical analysis
are undertaken by ALS Global at its laboratories in Karaganda
(Kazakhstan) and Loughrea (Republic of Ireland), respectively.
A 30 g split of the pulp is analyzed for gold
content by fire assay with an Atomic Absorption Spectroscopy (AAS)
finish (ALS method: Au-AA25™) at ALS Karaganda. A second pulp split
is then air freighted to ALS Loughrea and analyzed for 48 elements
by Inductively Coupled Plasma Mass Spectrometry (ICP-MS) after
four-acid digestion on a 0.25 g aliquot (ALS method: ME-MS61™). Any
samples exceeding 1% copper are re-analyzed using a 4-acid digest
ICP-MS ore grade method (ALS method: Cu-OG62™).
Arras Minerals operates according to its
rigorous internal Quality Assurance and Quality Control (QA/QC)
protocols, which are consistent with industry best practices. This
includes the insertion of certified standards, blanks, and field
duplicates comprising of quarter drill core into the sample stream
at an insertion rate of 2.5%, 2.5%, and 5%, respectively, which is
deemed appropriate for this stage of exploration. The blanks and
standards are Certified Reference Materials (CRM’s) supplied by Ore
Research and Exploration, Australia.
Internal QA/QC samples are also inserted by the
analytical laboratories and reviewed by the Company prior to
release.
Qualified Person: The technical
information of this news release has been reviewed and approved by
Tim Barry, a Chartered Professional Geologist MAusIMM CP(Geo), and
a qualified person for the purposes of National Instrument
43-101.
On behalf of the Board of Directors
"Tim Barry" Tim Barry, MAusIMM (CP(Geo))Chief Executive Officer
and Director INVESTOR RELATIONS: +1 604 687 5800
info@arrasminerals.com
Further information can be found on the Company’s website
https://www.arrasminerals.com or follow us on LinkedIn:
https://www.linkedin.com/company/arrasminerals
About Arras Minerals Corp.
Arras is a Canadian exploration and development
company advancing a portfolio of copper and gold assets in
northeastern Kazakhstan, including the Option Agreement on the
Beskauga copper and gold project. The Company has established the
third-largest license package in the country (behind Rio Tinto and
Fortescue Metals Group) prospective for copper and gold in the
country. The Company’s shares are listed on the TSX-V under the
trading symbol “ARK”.
Cautionary Note to U.S. Investors
concerning estimates of Measured, Indicated, and Inferred
Resources: This press release uses the terms “measured
resources”, “indicated resources”, and “inferred resources” which
are defined in, and required to be disclosed by, NI 43-101. The
Company advises U.S. investors that these terms are not recognized
by the SEC. The estimation of measured, indicated and inferred
resources involves greater uncertainty as to their existence and
economic feasibility than the estimation of proven and probable
reserves. U.S. investors are cautioned not to assume that measured
and indicated mineral resources will be converted into reserves.
The estimation of inferred resources involves far greater
uncertainty as to their existence and economic viability than the
estimation of other categories of resources. U.S. investors are
cautioned not to assume that estimates of inferred mineral
resources exist, are economically mineable, or will be upgraded
into measured or indicated mineral resources. Under Canadian
securities laws, estimates of inferred mineral resources may not
form the basis of feasibility or other economic studies.
Disclosure of “contained ounces” in a resource
is permitted disclosure under Canadian regulations, however the SEC
normally only permits issuers to report mineralization that does
not constitute “reserves” by SEC standards as in place tonnage and
grade without reference to unit measures. Accordingly, the
information contained in this press release may not be comparable
to similar information made public by U.S. companies that are not
subject NI 43-101.
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 U.S. Private Securities Litigation Reform Act of 1995, the
Securities Act of 1933, as amended, and the Exchange Act, and
applicable Canadian securities laws. Forward-looking statements
include, among others, statements regarding the use of net proceeds
from the recent private placement, plans and expectations of the
drill program Arras is in the process of undertaking, including the
expansion of the Mineral Resource, and other aspects of the Mineral
Resource estimates for the Beskauga project. These statements are
based on current expectations, estimates, forecasts, and
projections about Arras’ exploration projects, the industry in
which Arras operates and the beliefs and assumptions of Arras’
management. Words such as “expects,” “anticipates,” “targets,”
“goals,” “projects,” “intends,” “plans,” “believes,” “seeks,”
“estimates,” “continues,” “may,” variations of such words, and
similar expressions and references to future periods, are intended
to identify such forward-looking statements. Forward-looking
statements are subject to a number of assumptions, risks and
uncertainties, many of which are beyond management’s control,
including undertaking further exploration activities, the results
of such exploration activities and that such results support
continued exploration activities, unexpected variations in ore
grade, types and metallurgy, volatility and level of commodity
prices, the availability of sufficient future financing, and other
matters discussed under the caption “Risk Factors” in the
Management Discussion and Analysis filed on the Company’s profile
on SEDAR on February 24, 2023 and in the Company’s Annual Report on
Form 20-F for the fiscal year ended October 31, 2022 filed with the
U.S. Securities and Exchange Commission filed on February 24, 2023
available on www.sec.gov. Readers are cautioned that
forward-looking statements are not guarantees of future performance
and that actual results or developments may differ materially from
those expressed or implied in the forward-looking statements. Any
forward-looking statement made by the Company in this release is
based only on information currently available and speaks only as of
the date on which it is made. The Company undertakes no obligation
to publicly update any forward-looking statement, whether written
or oral, that may be made from time to time, whether as a result of
new information, future developments, or otherwise.
Photos accompanying this announcement are available at
https://www.globenewswire.com/NewsRoom/AttachmentNg/f441116d-88e1-4c0d-afcb-beb743e8a603
https://www.globenewswire.com/NewsRoom/AttachmentNg/8ecc6364-3ce4-4207-ad62-3e534a270756
https://www.globenewswire.com/NewsRoom/AttachmentNg/c40008a9-a72c-47c0-afac-c4c425f6a1d0
https://www.globenewswire.com/NewsRoom/AttachmentNg/c322abcc-ab52-4634-8e05-a0bf8f92e552
https://www.globenewswire.com/NewsRoom/AttachmentNg/b0692b3f-afdf-4c9b-8129-de05ac01a565
Arras Minerals (TSXV:ARK)
Historical Stock Chart
From Dec 2024 to Jan 2025
Arras Minerals (TSXV:ARK)
Historical Stock Chart
From Jan 2024 to Jan 2025