Arras Minerals Corp. (TSX-V: ARK) (“Arras” or “the
Company”) is pleased to announce assay results from holes
Bg21003 and Bg21004 from the ongoing drill program at the Beskauga
copper-gold deposit and surrounding area (“Beskauga” or the
“Project”).
Highlights:
- Hole Bg21004 returned a significant
intersection of 1120.4 meters of mineralization grading
0.59 % copper-equivalent (“CuEq”) or 0.73 g/t
gold-equivalent (“AuEq”) (0.39 g/t gold
(“Au”), 0.25 % copper (“Cu”), 1.31 g/t silver (“Ag”) and 22.3 ppm
molybdenum (“Mo”)) starting at 43.9 meters from surface to end of
hole.
- Including 465.1 meters grading 0.81 % CuEq
or 1.00 g/t AuEq (0.52 g/t Au, 0.36 % Cu, 1.70 g/t
Ag and 25.6 ppm Mo) from 43.9 meters depth down-hole.
- And including 35 meters grading 0.76 % CuEq or 0.94 g/t
AuEq (0.46 g/t Au, 0.37 % Cu, 2.0 g/t Ag and 26.2 ppm Mo)
from 741 meters depth down-hole.
- And including 207 meters grading 0.73 % CuEq or 0.90
g/t AuEq (0.55 g/t Au, 0.26 % Cu, 1.68 g/t Ag and 23.7 ppm
Mo) from 863 meters depth down-hole.
- The hole demonstrates the continuity of high-grade
mineralization to depth, up to 460 m beneath the base of the block
model of Arras’ recently announced Mineral Resource
Estimate for Beskauga (see Arras’ news
release dated June 20, 2022). The hole was terminated at a depth of
1164.3 m due to the capacity of the drill rig and ended in
porphyry-style mineralization with mineralization remaining open at
depth.
- The top of Hole Bg21003 returned 83.1
meters of mineralization grading 0.51% CuEq (0.33 g/t Au,
0.23 % Cu, 1.19 g/t Ag, and 13 ppm Mo) starting at 49.5 meters from
surface before the hole entered an unmineralized post-mineral
porphyritic diorite.
- Drilling is ongoing at Beskauga with further assay results
expected in the coming weeks.
Commenting on the results, Tim Barry, CEO of
Arras stated, “When considering the copper-equivalent grade
multiplied by the length of the intercept, hole Bg21004 represents
one of the best holes ever drilled on the Beskauga property, second
only to hole Bg21001 that returned an impressive 973.2 meters @
0.82 % CuEq [for further details, see Arras’ press release dated
January 31, 2022]. Perhaps more significantly, hole Bg21004 drilled
460 m below the base of our current resource block model,
substantially expanding the potential volume of high-grade
mineralization to depth in the southwest part of the main deposit.
Our Beskauga project continues to deliver, demonstrating the
large-scale characteristics of the deposit. We expect further drill
assays to be finalized over the coming weeks which we will report
as they become available.”
A summary of the results announced in this news
release is outlined in the table below.
Table
1. Summary table for holes Bg21003 and
Bg21004.
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%.
Drill Program: In October 2021,
Arras announced the start of a planned 30,000-meter diamond drill
program targeting the extensions of the Beskauga deposit both
laterally and at depth (see Figure 1). The drill program is being
conducted under the Option to Purchase agreement (“Option
Agreement”) executed on January 26, 2021, with Copperbelt AG
(“Copperbelt”), a private mineral exploration company registered in
Zug, Switzerland.
In addition to testing the extents of the
Beskauga deposit, the drilling program is also targeting a series
of previously undrilled targets in the wider area. These wider
targets are supported by both ground and recently flown airborne
geophysics, as well as in-situ geochemistry, derived using “KGK”
drilling (a drilling method akin to 'wet' reverse circulation
drilling, that recovers a 1-3 m core sample from the top of the
underlying bedrock which is used by Arras to efficiently map
lithology, alteration, and geochemistry across the property beneath
overburden).
For both the diamond and KGK drilling, Arras is
using the local company “Tsentrgeolsemka LLP”. Tsentrgeolsemka LLP
is independent of Arras. Arras plan to mobilize diamond drill rigs
with the capacity to drill deeper to enable the Company to fully
evaluate the continuation of the high-grade mineralization to
depth.
Results:
Bg21003 was collared 340 m
south-west of Bg21004 and drilled at an angle of -70 o towards the
south to a final depth of 404.7 m. The hole was designed to test a
clustering of Au-Cu-As-Bi anomalies within top of bedrock samples
retrieved through historical KGK drilling by Copperbelt. The hole
started in reasonably strong mineralization, up to 0.8 g/t Au, 0.62
% Cu, 2.45 g/t Ag, and 75 ppm Mo within a diorite with strong to
very strong argillic alteration comprising of illite and smectite
with subordinate kaolinite, before entering an unmineralized
post-mineral xenolithic porphyritic diorite dyke with strong to
moderate argillic alteration at a depth of 132.6 to 185.3 meters
down-hole. After the porphyritic diorite dyke, the hole entered a
weakly porphyritic, moderately argillic altered late-mineral
diorite variant with very weak mineralization (with sporadic higher
grades up to 0.75 % CuEq, dominated by copper over gold) in which
the hole was terminated. The porphyritic diorite dyke is
interpreted to have filled a pre-existing E-W trending fault zone
that has juxtaposed the strongly Cu-Au mineralized diorite of the
main Beskauga deposit to the north, with a distinct weakly
mineralized diorite variant to the south and may have structurally
offset the southern portion of the orebody. The presence of two
distinct diorite variants is further supported by trace element
lithogeochemistry.
Bg21004 (see Figures 2 and 3)
was collared 100 m west of Bg21001 (for results of Bg21001, refer
to Arras’ press release dated January 31, 2022), and drilled at an
angle of -70 o towards the south to a final depth of 1164.3 m where
it was terminated due to maximum depth capacity of the drill rig.
The mineralization observed in hole Bg21004 is hosted within a
sodic (strong albite alteration with a characteristic reddening
caused by hematite dusting**) altered diorite that has been later
overprinted by moderate, to very strong, argillic alteration
comprising of illite and smectite; with subordinate kaolinite and
dickite present at shallow levels (confirmed by Arras using
TerraSpec SWIR/NIR spectroscopy). Mineralization occurs as a
mixture of disseminated, vein, and fracture-controlled zones of
chalcopyrite, tennantite, and pyrite with minor bornite, covellite,
and molybdenite. Zones of sheeted and/or intense stockwork
quartz-Cu sulfide veins correlate with high-grade gold and copper
assays up to 4.5 g/t Au and 3.01 % Cu, respectively (see Figure 4).
Higher Mo grades up to 833 ppm occur sporadically but are more
abundant in the deepest parts of the hole. An unmineralized
post-mineral, yet argillic altered, xenolithic porphyritic diorite
dyke was intersected in two intercepts at depths of 586.85 to 623.7
meters and 640.5 to 715.0 meters down-hole. When removing the grade
dilution resulting from the unmineralized dyke, it leaves a
residual intercept of 1010.4 meters of mineralization grading 0.65
% CuEq or 0.80 g/t AuEq within the mineralized diorite.
** Sodic (and potassic) alteration in many
alkalic porphyry systems is characterized by hematite dusting of
feldspars and the zone of “reddening” can provide a useful vector
toward mineralization. In alkalic porphyry systems, sodic
alteration can occur in the upper levels of the system, which is in
accord with the epithermal overprinting observed within the
Beskauga deposit. Arras recently initiated petrological and
lithogeochemical studies to fully characterize the alteration,
evaluate the alkalic or high-K calc-alkaline nature of the Beskauga
deposit, and inform continued exploration.
Figure
1. Location of the holes completed to date
as part of Arras’ planned 30,000 meter drill program on the
Beskauga Main deposit and the wider area.
Figure 2. Cross-section showing hole
Bg21004 in relation to several historical holes drilled by
Copperbelt. 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 releases on June 20,
2022). CuEq grades of key intercepts in Bg21004 and historical
holes are shown. Note that hole Bg21004 demonstrates the continuity
of high-grade mineralization to depth, up to 460 m beneath the base
of the current block model. The cross-section demonstrates the
steep, southeast dipping high-grade copper-gold-silver trend
observed through Arras’ exploration to date. This trend is observed
beginning at the paleo-bedrock surface (44m in depth), to average
between 200-300m wide and to be consistently mineralized down to at
least 1000 meters. Mineralization remains untested at
depth.
Figure 3. Cross-section showing hole
Bg21004 in relation to several historical holes drilled by
Copperbelt. Also shown are grade contours based on the Beskauga
block model for gold (only) developed for the
purposes of the current Mineral Resource Estimate for Beskauga (for
further details, please see Arras’ press releases on June 20,
2022). AuEq grades of key intercepts in Bg21004 and historical
holes are shown. Note that hole Bg21004 demonstrates the continuity
of high-grade mineralization to depth, up to 460 m beneath the base
of the current block model. The cross-section demonstrates the
steep, southeast dipping high-grade copper-gold-silver trend
observed through Arras’ exploration to date. This trend is observed
beginning at the paleo-bedrock surface (44m in depth), to average
between 200-300m wide and to be consistently mineralized down to at
least 1000 meters. Mineralization remains untested at
depth.
Figure 4. Photos of the diamond drill
core from Bg21004 showing the typical styles of veining,
mineralization and alteration observed throughout the
hole.
About the Beskauga Deposit:
The Beskauga deposit is a gold-copper-silver
deposit with a NI 43-101 compliant “Indicated” Mineral Resource of
111.2 million tonnes grading 0.49 g/t gold, 0.30% copper, and 1.34
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 1.14 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. This
resource is based on 122 drill holes completed between 2007 and
2021. For further details regarding the Mineral Resource estimate
at the Beskauga project, please see the technical report entitled
“Beskauga Copper-Gold Project, Pavlodar Province, the Republic of
Kazakhstan," dated February 20, 2022, and filed on the Company’s
website and on the Company’s SEDAR profile at www.sedar.com.
The constraining pit was optimized and
calculated using an NSR cut-off based on a price of: $1,750/oz for
gold, $3.50/lb for copper, $22.00/oz for silver, and with an
average recovery of 85% for copper and 74.5% for gold and 50% for
silver.
Based on exploration undertaken to date, the
Beskauga deposit is interpreted by Arras to represent a gold-rich
porphyry copper-gold deposit that has been overprinted by
high-sulfidation epithermal mineralization, either through
telescoping or due to clustering of multiple porphyry centers
within the Beskauga license that have superimposed alteration and
mineralization upon earlier phases. Beskauga is located within the
highly under-explored Bozshakol-Chingiz Volcanic Arc, which hosts
KAZ Minerals’ Bozshakol porphyry Cu-Au mine only 130 km west of
Beskauga. Bozshakol is one of the largest copper resources in
Kazakhstan with 1.123 billion tonnes at 0.35% Cu, 0.14 g/t Au and
1.00 g/t Ag in Measured and Indicated Resources. The mine has a 30
Mtpa ore processing capacity and a remaining mine life of >40
years.
Contrary to many porphyry copper deposits being
developed in other jurisdictions globally, the Beskauga project
benefits from excellent modern infrastructure and accessibility and
is located at 350m above sea level. The region is mining-friendly
and hosts several large-scale mining operations. Arras’ operations
are based out of the nearby mining town of Ekibastuz, which
services the largest coal mine in Kazakhstan and provides a highly
trained workforce for the Company to draw upon. Paved road access,
1100 KVA power lines, heavy rail, and the Irtysh–Karaganda
irrigation canal all lie within a 25-kilometer radius of the
project. The capital city of Nur-Sultan, located approximately 300
kilometers along a four-lane highway to the west of the project,
has a major international airport allowing for easy access and
administration of the Beskauga project.
Assay and QAQC Procedures:
Diamond drill core was sampled in 1-meter
intervals (except were shortened by geological contacts) using a
rock saw. Core diameter is a mix of HQ and NQ depending on the
depth of the drill hole. Samples were cut and sampled at Arras’
operational base in the town of Ekibastuz, Kazakhstan by Company
personnel. All sample preparation and geochemical analysis of the
diamond drill core were undertaken by ALS Global at its
laboratories in Karaganda (Kazakhstan) and Loughrea (Republic of
Ireland), respectively. ALS Global is an accredited laboratory that
is entirely independent of the Company.
After drying and fine crushing, a 250 g split
was pulverized to 85 % passing a -75-micron screen. A 30 g split of
the pulp was analyzed for gold using fire assay and Atomic
Absorption Spectroscopy (AAS) finish (ALS method: Au-AA25™) at ALS
Karaganda. A second pulp split was then air freighted to ALS
Loughrea and analyzed for 48 elements by Inductively Coupled Plasma
Mass Spectrometry (ICP-MS) after 4-acid digestion on a 0.25 g
aliquot (ALS method: ME-MS61™). Samples exceeding 1% copper were
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 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 were also inserted
by the analytical laboratories and reviewed by the Company prior to
release. No material QA/QC issues have been identified with respect
to sample collection, security, and assaying.
Qualified Person:
The scientific and technical disclosure for the
Beskauga Project included in this news release has been reviewed
and approved by Joshua Hughes, the Vice President Exploration, and
a full-time employee of Arras Minerals Corp., who is also a Member
and Chartered Professional Geologist (MAusIMM CP(Geo)) of the
Australasian Institute of Mining and Metallurgy, a Fellow of the
Society of Economic Geologists (FSEG) and a Fellow of the
Geological Society of London (FGS). Mr Hughes has sufficient
experience, relevant to the styles of mineralization and type of
deposits under consideration and to the activity that he is
undertaking, to qualify as 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
About Arras Minerals Corp.
Arras Minerals Corp. is British Columbia
incorporated public company trading on the TSX-V exchange under the
symbol “ARK.” The Company is advancing a portfolio of copper and
gold assets in northeastern Kazakhstan, including an Option
Agreement on the Beskauga copper and gold project. Further
information can be found on the Company’s website
www.arrasminerals.com or follow us on LinkedIn:
https://www.linkedin.com/company/arrasminerals
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
Non-Offering Prospectus filed on the Company’s profile on SEDAR on
May 31, 2022 and in the Company’s Annual Report on Form 20-F for
the fiscal year ended October 31, 2021 filed with the U.S.
Securities and Exchange Commission filed on February 17, 2022
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/2b358878-ea6b-4946-9f92-f1e79e451a6b
https://www.globenewswire.com/NewsRoom/AttachmentNg/33c63c38-9718-45d2-9e0e-7a7f0594d8f3
https://www.globenewswire.com/NewsRoom/AttachmentNg/b87876d4-c916-4548-8e9c-143abbe7ae1e
https://www.globenewswire.com/NewsRoom/AttachmentNg/2c5eb8a9-61ba-425e-841b-355f1ac2aab8
https://www.globenewswire.com/NewsRoom/AttachmentNg/49c1fee9-7e5b-4895-b56a-e9ccf729b505
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