Copper Fox Metals Inc.
(“Copper Fox” or the “Company”)
(TSX-V: CUU – OTC-Pink: CPFXF) and its wholly owned
subsidiary, Desert Fox Copper Inc., are pleased to provide
additional analytical results for the recently completed mapping
and sampling program on its 100% owned Mineral Mountain copper
project located approximately 15 miles east of Florence, Arizona.
Highlights:
- A large area of copper-molybdenum
mineralization has been located in the southeast corner of Area #1
with molybdenum concentration of up to 0.2%.
- The copper mineralization in Area
#1 and Area #3 has been extended and remains open in several
directions.
- The mineralization in Area #2
occurs within a narrow, northeast trending zone estimated to be 2.8
kms long.
- Two new areas of significant copper
mineralization have been located in the Laramide age
intrusive.
Elmer B. Stewart, President and CEO of Copper
Fox, stated, “Following the significant results from the initial
sampling program, the recent results continue to expand the limits
of the copper mineralization in Areas #1 and #3; and more
importantly, has identified a large area of copper-molybdenum
mineralization in the southeast corner of Area #1 along the
Laramide/Precambrian intrusive contact. Results for the balance of
the samples collected during the recently completed Phase 2
sampling program will be released on receipt thereof.”
Geological Model:
The surface mineralization represents weathered
porphyry copper mineralization (a “leach cap”) sitting above a
buried porphyry copper system (see news release dated April 30,
2018). The recent mapping program has located a number of intrusive
phases in the Laramide age intrusive that are not shown on the
preliminary geology map covering the project area. The sulfur
content of the samples strongly supports the leached nature of the
Laramide age intrusive that hosts the majority of the copper
mineralization.
Analytical Results:
The mapping and sampling program consisted of
mapping lithologies, alterations, and vein assemblages. Selected
rock chip samples were collected from mineralized outcrops to
characterize the metals present in veins, other mineralized
structures and the outcrop. The samples are not necessarily
representative of the mineralization on the property. Outcrop
exposures within the sampled area are estimated to 5-10%. The
approximate dimensions and average metal concentrations in the
Areas sampled for the current analytical results are tabulated
below (see tables below for individual sample results). The average
concentrations of the metals by Area included in this news release
do not include the analytical results discussed in the November 21,
2018 news release.
|
|
|
|
|
|
|
|
|
Average Concentration |
Area |
# of
samples |
Length
(m) |
Width
(m) |
Cu
(ppm) |
Cu
(%) |
Mo
(ppm) |
Mo
(%) |
Au
(ppb) |
Ag
(ppm) |
1 |
26 |
1,200 |
800 |
7,584 |
0.758 |
203.0 |
0.020 |
95.0 |
26.8 |
2 |
7 |
1,200 |
400 |
9,419 |
0.942 |
50.4 |
0.005 |
18.4 |
21.8 |
3 |
13 |
800 |
500 |
6,946 |
0.694 |
13.0 |
0.001 |
65.1 |
3.7 |
Cu = copper, Mo = molybdenum, Au = gold, Ag
=silver, (%) = percent, ppm = parts per million,
ppb = parts per billion |
|
Area #1:
The copper mineralization has been extended
approximately 200m to the west and 400m to the south and southeast
and remains open to the west and to the south towards Area #3.
Sampling 1.6 kms to the east of Area #1 located a new area of
copper mineralization hosted in the Laramide age Quartz Monzonite
intrusive. The ground between Area #1 and the new discovery has
been mapped and analytical results for the samples collected during
this work are pending. The additional analytical results for
mineralized samples collected from Area #1 are shown below:
|
|
|
|
|
|
|
|
|
|
|
|
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
MM-393 |
1800 |
0.180 |
5.2 |
8 |
2.3 |
MM-384 |
8290 |
0.829 |
3.9 |
10 |
21.6 |
MM-394 |
2310 |
0.231 |
2.6 |
6 |
6.4 |
MM-385 |
5790 |
0.579 |
8.0 |
5 |
6.1 |
MM-395 |
1380 |
0.138 |
1.5 |
41 |
28.9 |
MM-386 |
16800 |
1.680 |
971.0 |
696 |
40.3 |
MM-398 |
4650 |
0.465 |
1.7 |
21 |
0.4 |
MM-387 |
20200 |
2.020 |
1060.0 |
8 |
14.1 |
MM-399 |
2080 |
0.208 |
17.8 |
5 |
0.8 |
MM-388 |
1740 |
0.174 |
8.3 |
10 |
1 |
MM-401 |
12100 |
1.210 |
732.0 |
98 |
14.2 |
MM-389 |
3230 |
0.323 |
49.5 |
24 |
2.8 |
MM-402 |
8470 |
0.847 |
4.3 |
9 |
5.0 |
MM-390 |
20900 |
2.090 |
2080.0 |
694 |
25.6 |
MM-403 |
18900 |
1.890 |
42.7 |
53 |
11.8 |
MM-408 |
2230 |
0.223 |
4.3 |
56 |
2.3 |
MM-404 |
227 |
0.027 |
0.5 |
9 |
0.2 |
MM-409 |
15200 |
1.520 |
8.4 |
169 |
12.7 |
MM-405 |
6600 |
0.660 |
31.8 |
5 |
1.6 |
MM-410 |
8880 |
0.880 |
158.0 |
13 |
3.5 |
MM-406 |
890 |
0.089 |
1.0 |
6 |
0.9 |
MM-411 |
3960 |
0.396 |
0.9 |
79 |
3.5 |
MM-382 |
22200 |
2.220 |
72.2 |
35 |
483.0 |
MM-413 |
435 |
0.044 |
0.1 |
5 |
0.5 |
MM-383 |
213 |
0.021 |
2.2 |
6 |
2.4 |
MM-414 |
7700 |
0.770 |
3.1 |
395 |
6.1 |
|
|
|
|
|
|
|
|
|
|
|
|
Area #2:
The additional sampling in this area indicates
that the mineralization is confined to a narrow, northeast trending
zone. Analytical results for mineralized samples from Area #2 are
shown below:
|
|
|
|
|
|
|
|
|
|
|
|
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
MM-356 |
208 |
0.021 |
6.1 |
11 |
3 |
MM-342 |
10600 |
1.060 |
282 |
15 |
6.1 |
MM-357 |
7540 |
0.754 |
4.6 |
10 |
4.8 |
MM-361 |
1420 |
0.142 |
44.4 |
23 |
6 |
MM-358 |
13900 |
1.390 |
8 |
37 |
83.2 |
MM-367 |
32100 |
3.210 |
3.1 |
5 |
40.8 |
MM-365 |
167 |
0.017 |
4.3 |
28 |
8.9 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Area #3:
The copper mineralization has been extended
approximately 400m to the south and mapping and prospecting
indicates that the mineralization is open to the north toward Area
#1 and to the south. A new area of copper mineralization has been
located approximately 600m west of Area #3 hosted in Laramide age
Quartz Monzonite intrusive. Analytical results for mineralized
samples collected in Area #3 are shown below:
|
|
|
|
|
|
|
|
|
|
|
|
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
Sample ID |
Cu (ppm) |
Cu (%) |
Mo (ppm) |
Au (ppb) |
Ag (ppm) |
MM-372 |
11400 |
1.14 |
98.4 |
45 |
4.5 |
MM-376 |
2320 |
0.232 |
1.2 |
<5 |
0.5 |
MM-373 |
12400 |
1.24 |
12.2 |
18 |
7.4 |
MM-377 |
9860 |
0.986 |
7.1 |
8 |
9.7 |
MM-374 |
1570 |
0.157 |
0.5 |
18 |
0.9 |
MM-378 |
7030 |
0.703 |
2.9 |
17 |
3.1 |
MM-364 |
4940 |
0.494 |
4.7 |
99 |
6.9 |
MM-379 |
19700 |
1.97 |
8.7 |
292 |
3.6 |
MM-370 |
1120 |
0.112 |
0.5 |
<5 |
0.4 |
MM-380 |
7490 |
0.749 |
0.6 |
<5 |
0.4 |
MM-371 |
6210 |
0.621 |
28.7 |
56 |
9.7 |
MM-444 |
2440 |
0.244 |
3.2 |
34 |
0.8 |
MM-375 |
3820 |
0.382 |
0.9 |
<5 |
0.7 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Mineralization:
The copper mineralization occurs in quartz
veins, veinlets and sheeted quartz veins (with and without potassic
alteration envelopes), as malachite-chalcocite and chalcocite veins
and veinlets (of variable thickness), on fractures and
disseminations hosted in potassic and phyllic altered Laramide age
Quartz Monzonite and porphyritic intrusives (containing 15-30%
phenocrysts). The main copper minerals are malachite, chrysocolla
and chalcocite with minor azurite, native copper and rare
chalcopyrite. Gangue minerals include goethite after pyrite and
jarosite.
Analytical and Sampling
Procedures:
Outcrop sampling as well as mapping lithologies,
alterations, and vein assemblages was completed. Selected rock chip
samples were collected from outcrop to characterize the metals
present in veins, other mineralized structures and the outcrop.
Outcrop exposures within the sampled area are estimated to 5-10%.
The samples were picked up from site by Skyline Laboratories of
Tucson, Arizona.
Samples were crushed to plus 75% -10 mesh, split
and pulverized to plus 95% -150 mesh. Pulps were subjected to a
multi-acid digest (HNO3, HF, and HClO4). Gold was analyzed on a
30-gram charge by fire assay (FA-01) with an atomic absorption
finish. Skyline’s package code TE-5 was used to analyze the samples
for the base and other trace elements. Metal concentration in
samples exceeding the upper limit of detection were assayed for
copper using (MEA) and silver (FA-04). Skyline has an ISO/IEC
17025/2005 accreditation.
Quality Control:
A total of 1 field blank and 5 certified
reference standards were inserted (insertion rate 1:17) with the
sample for which analyses are being reported. QA/QC shows that the
blank and standards were within +/-5% of accepted value for the
blank and standards.
Elmer B. Stewart, MSc. P. Geol., President and
CEO of Copper Fox, is the Company’s non-independent, nominated
Qualified Person pursuant to National Instrument 43-101, Standards
for Disclosure for Mineral Projects, and has reviewed and approves
the scientific and technical information disclosed in this news
release.
About Copper Fox:
Copper Fox is a Tier 1 Canadian resource company
listed on the TSX Venture Exchange (TSX-V: CUU) focused on copper
exploration and development in Canada and the United States. The
principal assets of Copper Fox and its wholly owned Canadian and
United States subsidiaries, being Northern Fox Copper Inc. and
Desert Fox Copper Inc., are the 25% interest in the Schaft Creek
Joint Venture with Teck Resources Limited on the Schaft Creek
copper-gold-molybdenum-silver project located in northwestern
British Columbia and a 100% ownership of the Van Dyke oxide copper
project located in Miami, Arizona. For more information on Copper
Fox’s other mineral properties and investments visit the Company’s
website at http://www.copperfoxmetals.com.
On behalf of the Board of Directors
Elmer B. StewartPresident and Chief Executive
Officer
|
|
|
For additional
information contact: |
|
|
Copper Fox Metals
Inc. |
|
Renmark Financial
Communications Inc. |
Lynn Ball:
investor@copperfoxmetals.com |
|
Robert Thaemlitz:
rthaemlitz@renmarkfinancial.com |
(844) 484-2820 or (403)
264-2820 |
|
Tel: (416) 644-2020 or
(514) 939-3989 |
www.copperfoxmetals.com |
|
www.renmarkfinancial.com |
|
|
|
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 release.
Cautionary Note Regarding
Forward-Looking Information:
This news release contains forward-looking
statements within the meaning of the Section 27A of the Securities
Act of 1933 and Section 21E of the Securities Exchange Act of 1934,
and forward-looking information within the meaning of the Canadian
securities laws (collectively, “forward-looking information”).
Forward-looking information is generally identifiable by use of the
words “believes,” “may,” “plans,” “will,” “anticipates,” “intends,”
“budgets”, “could”, “estimates”, “expects”, “forecasts”, “projects”
and similar expressions, and the negative of such expressions.
Forward-looking information in this news release includes
statements regarding: the copper-molybdenum mineralization in the
southeast corner of Area #1; molybdenum concentrations of up to
0.2%; releasing the remaining results of Phase 2 sampling; the
approximate dimensions of the mineralized zones and average
concentrations of the metals for the target areas and two
additional areas of significant copper mineralization; and the
leached nature of the Laramide age intrusive that hosts the
majority of the copper mineralization.
In connection with the forward-looking
information contained in this news release, Copper Fox and its
subsidiaries have made numerous assumptions regarding, among other
things: the geological advice that Copper Fox has received is
reliable and is based upon practices and methodologies which are
consistent with industry standards and the reliability of
historical reports; and receipt of the remaining results from the
Phase 2 sampling program. While Copper Fox considers these
assumptions to be reasonable, these assumptions are inherently
subject to significant uncertainties and contingencies.
Additionally, there are known and unknown risk
factors which could cause Copper Fox’s actual results, performance
or achievements to be materially different from any future results,
performance or achievements expressed or implied by the
forward-looking information contained herein. Known risk factors
include, among others: the dimensions and shape of the mineralized
areas may not be as estimated; the additional samples may be
delayed or may not yield significant concentrations of metals;
additional sampling may not locate copper mineralization; the
surface mineralization may not represent buried porphyry style
mineralization; uncertainties relating to interpretation of the
outcrop sampling results; the geology, continuity and concentration
of the mineralization; the financial markets and the overall
economy may deteriorate; the need to obtain additional financing
and uncertainty of meeting anticipated program milestones;
uncertainty as to timely availability of permits and other
governmental approvals.
A more complete discussion of the risks and
uncertainties facing Copper Fox is disclosed in Copper Fox's
continuous disclosure filings with Canadian securities regulatory
authorities at www.sedar.com. All forward-looking information
herein is qualified in its entirety by this cautionary statement,
and Copper Fox disclaims any obligation to revise or update any
such forward-looking information or to publicly announce the result
of any revisions to any of the forward-looking information
contained herein to reflect future results, events or developments,
except as required by law.
Copper Fox Metals (TSXV:CUU)
Historical Stock Chart
From Dec 2024 to Jan 2025
Copper Fox Metals (TSXV:CUU)
Historical Stock Chart
From Jan 2024 to Jan 2025