VANCOUVER, BC, Nov. 16,
2023 /CNW/ - Cascadia Minerals Ltd.
("Cascadia") (TSXV: CAM) is very pleased to provide results
of the first two diamond drill holes ever completed at
its 100%-controlled flagship Catch Property in central Yukon, Canada, located 16 km from an
all-season highway and powerline within the traditional territory
of the Little Salmon Carmacks First Nation. The Catch Property
hosts multiple new greenfield discoveries of copper-gold
porphyry mineralization within the northern extension of the
prolific Stikine Terrane from BC's Golden Triangle. A total of five
holes were drilled at Catch in 2023, totalling 2,462 m. This release contains results from the
first two holes (1,066 m), with
results from the remaining three holes pending.
Drilling Highlights
- First diamond holes ever drilled at the Catch
property both yielded significant copper-gold
mineralization, confirming a new copper-gold porphyry
discovery;
- Hole CA-23-002 intersected 116.60
m of 0.31% copper and 0.30 g/t gold from 356.00 m downhole, within a broader interval of
435.00 m of 0.16% copper and
0.09 g/t gold (Figures 1-3);
- Hole CA-23-001 intersected 45.83
m of 0.30% copper and 0.15 g/t gold from surface, within
a broader interval of 333.87 m of
0.13% copper (Figures 1-3);
- These holes were drilled 160 m
apart, in the middle of coincident 1,200 x 600 m chargeability and 800 x 600 m magnetic anomalies that are just
beginning to be tested (Figures 1-3);
- Drilling has yet to intersect significant potassic
alteration, suggesting there is potential to discover higher
copper and gold grades in the untested core of the porphyry
system;
- Results are pending from three additional diamond drill
holes at the Main Zone, located 2 km north of these
drill holes (Figure 1); and
- Cascadia invites shareholders and other interested parties to
attend a video webinar and technical Q&A to be held
Friday, November 17th at
8:00 AM PT / 11:00 AM ET to learn more about the
significance of these results: Register Here.
"To have made a significant copper-gold porphyry discovery in
the first two holes ever drilled on a project is incredibly rare.
We can now focus on expanding known mineralization and exploring
for even higher-grade zones, whilst simultaneously testing numerous
additional targets," said Graham
Downs, Cascadia's President and CEO. "Our second hole
returned over a hundred metres of 0.31% copper and 0.30 g/t gold,
comparable to the resource grade of Newmont's operating Red Chris
open-pit mine in BC's Golden Triangle (Measured and Indicated
open-pit grade of 0.34% copper and 0.28 g/t gold*). We
have clearly tapped into a large porphyry system and eagerly await
results from the remaining three holes that were drilled at the
Main Zone, 2 km to the north. Cascadia is the first mover in
the underexplored extension of the Stikine Terrane in Yukon, and we will utilize Catch as a case
study regionally to acquire additional land throughout this
compelling new porphyry district, as we prepare for an early 2024
drill program at Catch."
*Red Chris resource grades are referenced from Newcrest
Mining Limited's (now Newmont Corporation) press release dated
March 31st, 2021.
Figure 1 – Catch Drilling Overview Map
Figure 2 – Diorite Zone Drill Map
Figure 3 – Diorite Zone Section
Figure 4 – Catch Location & Infrastructure
Figure 5 – Stikine Terrane Map
Catch Property Drilling
Summary
The first two diamond drill holes at the Catch Property were
completed at the Diorite Zone. Hole CA-23-001 ended at 511.83 m depth and Hole CA-23-002 ended at
554.00 m depth, with sulphide
mineralization (pyrite-pyrrhotite-chalcopyrite) observed to the end
of both holes. Both holes were targeting a broad Induced
Polarization ("IP") chargeability anomaly at depth, underlying
coincident high-grade surface mineralization, within a pronounced
magnetic anomaly. An additional three holes were drilled at the
Main Zone, located 2 km north, and results from these holes are
pending.
Table 1: 2023 Catch Assays Result Summary
Drill
Hole
|
From
(m)
|
To
(m)
|
Interval
(m)*
|
Copper
(%)
|
Gold
(g/t)
|
CA -23-001
|
14.00
|
347.87
|
333.87
|
0.13
|
0.04
|
incl.
|
14.00
|
59.83
|
45.83
|
0.30
|
0.15
|
CA
-23-002
|
80.00
|
515.00
|
435.00
|
0.16
|
0.09
|
incl.
|
356.00
|
472.60
|
116.60
|
0.31
|
0.30
|
and incl.
|
357.93
|
362.00
|
4.07
|
0.51
|
6.03
|
and incl.
|
407.00
|
472.60
|
65.60
|
0.40
|
0.13
|
* The reported
intervals are drilled thicknesses and true widths are
unknown.
|
Hole CA-23-001 targeted a high IP chargeability anomaly
underlying an outcrop which returned 0.31% copper with 0.17 g/t
gold over 12 m from a hand trench.
The hole encountered basalt, diorite and gabbro host rocks. Copper
and gold mineralization is associated with propylitic
(chlorite-albite-epidote-calcite) to sodic (albite-chlorite-pyrite)
alteration of all host rock types that carry quartz-carbonate ±
pyrite-chalcopyrite veins and disseminated to blebby pyrite,
pyrrhotite and chalcopyrite (sulphides listed in decreasing order
of abundance). The hole ended in anomalous copper grades, with
visual pyrrhotite and pyrite mineralization noted.
Hole CA-23-002 was collared 160 m
north of CA-23-001, targeting the same high IP chargeability
anomaly, underneath an outcrop which returned high-grade grab
samples including 3.88% copper with 30.00 g/t gold. The hole
encountered similar rock types, alteration and mineralization to
hole 001, in addition to localised quartz-feldspar porphyry dykes
up to 17 m in width, and an overall
increase in copper and gold grades. The hole ended in anomalous
copper grades, with visual pyrrhotite and pyrite mineralization
noted.
Drilling has not yet intersected significant potassic
alteration, suggesting there is potential to discover higher copper
and gold grades associated with the potassic core of the system.
Additional drilling will be required to vector towards this core.
Both holes were drilled in the middle of a coincident 1,200 x
600 m high IP chargeability anomaly
and 800 x 600 m magnetic low anomaly.
These geophysical features have provided a valuable vector towards
mineralization and remain open in all directions.
Table 2: 2023 Catch Drill Hole Collars**
Drill
Hole
|
Easting
(m)
|
Northing
(m)
|
Azimuth
(°)
|
Dip
(°)
|
Depth
(m)
|
CA-23-001
|
482,726
|
6,859,800
|
130.4
|
-60
|
511.83
|
CA-23-002
|
482,702
|
6,859,958
|
129.7
|
-65
|
554.00
|
** Easting and Northing
are UTM co-ordinates in the NAD 83 datum, zone 8N. Azimuth is with
respect to true north.
|
Soil sampling was also completed across the Catch property to
evaluate newly staked areas, with a total of 830 soil samples
collected. Multiple anomalies were identified that will be
followed-up with prospecting and mapping next exploration
season.
Property Geology and
Mineralization
The 71 km2 Catch Property is in central
Yukon, Canada, 56 km southeast of
the town of Carmacks (Figure 4),
in an underexplored part of the Stikine Terrane – which extends
from the Golden Triangle in British
Columbia into Yukon (Figure
5), where it is immediately adjacent to the 1,000+ km long, deep
seated, crustal scale strike-slip Teslin-Thibert fault. The Stikine
Terrane is characterized by Late Triassic to early Jurassic
volcanic-plutonic arc complexes that are well-endowed with
copper-gold-molybdenum porphyries including the Red Chris, Schaft
Creek, Kemess, KSM and Galore Creek deposits and mines. The
property is located wholly within the traditional territory of the
Little Salmon Carmacks First Nation.
The Catch area is mostly underlain by augite phyric basalt of
the Semenof Formation, centered on a 7 x 3 km regional magnetic
high. Mineralization is associated with propylitic to sodic
alteration of basalt and lesser diorite, intrusion-cemented and
hydrothermal breccias. Locally there is intense albitization,
silicification, brecciation and up to 10% disseminated to blebby
pyrite, chalcopyrite and trace bornite and pyrrhotite. Secondary
copper minerals including malachite, azurite and tenorite are
widespread at surface, coat fracture surfaces, and are often
associated with gypsum.
The geology, alteration and mineralization observed throughout
Catch are all indicative of a significant copper-gold ± molybdenum
bearing porphyry system.
Catch is under option from a Yukon prospector, and Cascadia can earn up to
a 100% interest, subject to a royalty. For more information, see
the Catch Property Technical Report filed on SEDAR+ at
www.sedarplus.ca under the Cascadia Minerals Ltd. profile, or
visit our website at www.cascadiaminerals.com for additional
maps and figures.
About Cascadia
Cascadia is a Canadian junior mining company focused on
exploring for copper and gold in Yukon and British
Columbia. Cascadia's flagship Catch Property is a brand-new
grassroots porphyry discovery which exhibits extensive high-grade
copper and gold mineralization across a 5 km long trend, with rock
samples returning peak values of 3.88% copper and 30.00 g/t gold
and initial drill results returning broad intervals of
mineralization, including 116.60 m of
0.31% copper with 0.30 g/t gold. In addition to Catch, Cascadia is
conducting exploration work at its PIL Property in British Columbia and the Sands of Time and
Rosy properties in Yukon, as well
as evaluating additional regional opportunities. Cascadia has
approximately 37 million shares outstanding and its largest
shareholders are Hecla Mining Company (19.8%) and Barrick Gold (7.6%).
QA/QC
Analytical work for samples was completed by ALS Canada Ltd,
with sample preparation in Whitehorse, Yukon and Langley,
BC, and geochemical analyses in North Vancouver, BC. Core samples were fine
crushed before a 250-gram split was pulverized to better than 85%
passing 75 microns. Gold was determined for core samples by the
PGM-ICP24 procedure which involves fire assay preparation using a
50-gram charge with an inductively coupled plasma-atomic emission
spectroscopy finish ("ICP-AES"). Soil samples were dry-screened at
180 micron, with analysis conducted on the fine fraction. Gold was
determined for soil samples by the Au-ICP21 method, which involves
fire assay preparation with a 30-gram charge followed by an ICP-AES
finish. Multi-element data for 48 elements was determined for all
samples by the ME-MS61 procedure, which involves a four-acid
digestion followed by ICP-AES and inductively coupled plasma-mass
spectrometry.
Rigorous procedures are in place regarding sample collection,
chain of custody and data entry. Certified assay standards,
duplicate samples and blanks are routinely inserted into the sample
stream of diamond drill samples to ensure integrity of the assay
process. All diamond drill samples included in this news release
have passed the QA/QC procedures as described above. All assay
intervals presented in this news release are uncut. Core was
sampled using a diamond saw, with half of each interval sent to the
lab for analysis, and the other half retained.
Results referenced in this release represent highlight results
only. Below detection values for gold and copper have been
encountered in drilling, rock and soil samples in these target
areas.
The technical information in this news release has been approved
by Adam Coulter, M.Sc., P.Geo., VP
Exploration for Cascadia and a qualified person for the purposes of
National Instrument 43-101.
On behalf of Cascadia Minerals Ltd.
Graham Downs, President and
CEO
NEITHER THE TSX VENTURE EXCHANGE NOR ITS
REGULATION SERVICES PROVIDER (AS THAT TERM IS DEFINED IN THE
POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY FOR
THE ADEQUACY OR ACCURACY OF THIS NEWS RELEASE.
Cautionary note regarding
forward-looking statements:
This press release may contain "forward-looking information"
within the meaning of applicable securities laws. Readers are
cautioned to not place undue reliance on forward-looking
information. Actual results and developments may differ materially
from those contemplated by these statements. The statements in this
press release are made as of the date of this press release. The
Company undertakes no obligation to update forward-looking
information, except as required by securities laws.
SOURCE Cascadia Minerals Ltd.