Halcones Precious Metals Corp. (TSX – V: HPM) (the
“Company” or “Halcones”) is pleased to announce assay results from
the initial 2022 exploration program at its Carachapampa project
(“Carachapampa” or the “Project”), Chile. Field mapping and rock
sampling were carried out in September, towards the end of the
South American winter and crews were successful in identifying well
mineralized zones in outcrop at several locations on the Project.
Highlights include:
- A new highly prospective target
area has been identified by the Company’s field program. Well
mineralized and strongly silicified (vuggy quartz textured)
structures have been discovered adjacent to a previously
unidentified volcanic dome. Presence of volcanic domes are
essential to development of the high sulfidation gold deposits in
this region.
- At least four structures
characterized by intense vuggy silica alteration were identified
initially, with gold values in bedrock samples of 17.2 g/t Au, 8.93
g/t Au, 4.2 g/t Au, 3.6 g/t Au and 1.43 g/t Au. This sampling is
based on limited exposure due to young volcanic cover in the area
and as well was hampered by intermittent snow cover when work was
done. More detailed mapping and sampling is in progress on this new
target presently.
- The structures have been mapped for
at least 600 metres along strike and across strike for more than
200 metres. Mapping is ongoing presently to identify additional
structures as well as to look for windows where the rocks between
the structures may be exposed through the cover of younger
volcanics in the area.
- Drill hole 003 which was drilled
previously appears to have collared on the side of the newly
identified volcanic dome and intercepted 54 m grading 0.32 g/t Au
including 20 m grading 0.56 g/t Au. This hole was drilled prior to
the mapping and does not intersect the mineralized structures but
is an indication of a highly anomalous and wide section of
mineralization associated with the flank of the dome. The hole is
approximately 1.5 km northeast from the mineralized samples.
- A second area approximately 1 km
north and still on the flank of the dome returned samples with 2.5
g/t Au and 65 g/t Ag on highly silicified, vuggy quartz altered
structures as well.
- One sample from the northeast
target area which occurs approximately 2.8 km northwest of this new
target area had a grade of 548 g/t Ag.
According to Vern Arseneau, COO of Halcones,
“The initial field results are highly encouraging. Given the
limited time the crews had in the field in the late winter, the
discovery of the previously unmapped volcanic dome and associated
vuggy silica alteration hosting significant gold mineralization
over what appears to be an extensive area is an excellent outcome.
Now that the weather has improved as Andean summer has commenced,
the crews are back in the field to follow up on the initial
discoveries with detailed sampling and mapping in preparation for
drill testing in the coming months.”
Paul Pint, CEO of Halcones noted “We are just
getting started with the work on this exciting Project, having only
had the property for a few months and much of that time during
Andean winter weather. It’s exciting to see the Project advancing
at this early stage in the program.”
Carachapampa Project
The Carachapampa Project is located in the
north-central part of the famous Maricunga Belt in Chile,
approximately 180 km northeast of the city of Copiapo (Figure 1).
The property is immediately adjacent to the past producing Nueva
Esperanza Au-Ag mine and north of Kinross Gold’s La Coipa
operations.
https://www.globenewswire.com/NewsRoom/AttachmentNg/7aa9c3de-b8fc-4a0e-96e3-3882a2170b59Figure
1: Location map, Carachapampa Project in the Maricunga
Belt.
The Carachapampa property is host to two
prominent volcanic domes which are considered an essential
component for development of high sulfidation gold deposits in this
area (Figure 2). The forces that drive the magma to surface also
drive large volumes of highly acidic fluids that are responsible
for dissolving rock forming minerals near surface and creating the
porous “vuggy quartz” alteration into which gold and silver
mineralization is subsequently deposited (Figure 3).
https://www.globenewswire.com/NewsRoom/AttachmentNg/2527bc60-c4c6-4c4d-ba5d-11581b984a54Figure
2: Photo mosaic showing the two large volcanic domes at
Carachapampa. The property boundary is shown in red. A third
smaller dome occurring between them was recently identified and
appears to have significant gold mineralization associated with
it.
https://www.globenewswire.com/NewsRoom/AttachmentNg/ba60c575-bd88-49f2-9b3e-260f640ced67Figure
3: Conceptual geological model illustrating the relationship
between volcanic domes and Au-Ag deposits in the area. Esperanza
Dome is associated with the Arqueros and Chimberos gold mines
located approximately 2 km west of the Carachapampa
property.
During Halcones’ initial field program,
geologists discovered a previously unidentified volcanic dome at
the central part of the property and adjacent to that have
discovered high grade mineralization in outcrops (Figure 4, 5, 6).
Subsequent mapping and sampling has identified an extensive area on
the west flank of the dome with strongly anomalous gold and locally
high silver in numerous samples. This area is the focus for present
field follow up with detailed mapping, sampling and targeted IP in
preparation trenching and drilling in in the coming months.
https://www.globenewswire.com/NewsRoom/AttachmentNg/480d79b8-5818-4f1b-8486-9394491eb548Figure
4: Map showing location of newly identified target area in the
circle on the west side of the Carachapampa Project. The newly
identified volcanic dome is enclosed in the dashed red line in the
northeast quadrant. Anomalous gold samples in bedrock and sub
outcrop are shown in red and yellow. Hole 003 referred to above is
shown on the flank of the dome.
https://www.globenewswire.com/NewsRoom/AttachmentNg/1440b056-2ab3-4fc2-b782-956489158c29Figure
5: At least four structures characterized by intense vuggy silica
alteration and associated gold mineralization were mapped over
approximately 600 metres of strike and across a width of
approximately 200 metres. Detailed work is ongoing presently to
attempt to expand on this potentially extensive mineralized
area.
https://www.globenewswire.com/NewsRoom/AttachmentNg/e718f641-da6a-4816-a0a4-27ee882221efFigure
6: Anomalous silver values also occur, primarily in the northern
part of the target area
Sampling Protocol
Sampling is conducted in a manner that will
allow reasonable averaging and statistical analysis of the data for
resource estimation. Standards, blanks and duplicate samples, are
used to maintain quality control and to verify laboratory
procedures. The company has established a QA/QC sampling control
protocol which it applies to all rock sampling, including chip
channels from trenches, surface grab samples and diamond drilling.
Following is a summary of these protocols:
Drilling:
- Samples are
collected using a standard 0.5 m to 1 m sample length in the main
mineralized zones and a 1 m to 2 m length in the surrounding rocks
or in other minor intervals of alteration and/or mineralization.
Shorter sample lengths were avoided whenever was possible.
- Core samples are
split along the core axis using an electric rock saw, by the
Company’s trained technicians, prior to sampling the core is logged
and a high-resolution photographic record is taken for the
files.
- One standard
sample is inserted for each 20 core samples and one coarse blank,
one fine blank and one internal duplicate sample are included each
50 core samples for QA/QC control.
- In order to meet
NI 43-101 security standards, the samples are placed in rice bags
and sealed with numbered security tags on site and then shipped to
the laboratory facilities by truck by Company personnel. The
custody and transfer of samples is always the responsibility of
Company personnel.
Surface and trenches:
- Channel trench
samples are collected using a standard 0.5 m to 1 m sample length
in the main mineralized zones and a 1 m to 2 m length in the
surrounding rocks or in other minor intervals of alteration and/or
mineralization. Shorter sample lengths are avoided whenever was
possible.
- Field mapping
samples are also collected using a standard 0.5 m to 1 m sample
length in mineralized zones when possible, depending on the outcrop
availability.
- One standard
sample is inserted for each 20 core samples and one coarse blank,
one fine blank and one internal duplicate sample are included each
50 samples for QA/QC control.
- In order to meet
NI 43-101 security standards, the samples are placed in rice bags
and sealed with numbered security tags on site and then shipped to
the laboratory facilities by truck by Company personnel. The
custody and transfer of samples is always the responsibility of
Company personnel.
Laboratory Analysis
All analyses of the samples were carried out by
ALS Limited, an independent laboratory with all regulatory
documents and certifications approved and up to date. The sample
prep facilities are based in Copiapo, 180 km SW from the
project.
The analysis package chosen, for Au, Ag, and a
multi-elements, trace level method are as follows:
Au-ICP21/Au-ICP22 – Fire Assay Fusion – ICP-AES
Finish Sample Decomposition: Fire Assay Fusion (FA-FUSPG1 &
FA-FUSPG2) Analytical Method: Inductively Couple Plasma – Atomic
Emission Spectrometry A prepared sample is fused with a mixture of
lead oxide, sodium carbonate, borax, silica and other reagents as
required, inquarted with 6 mg of gold-free silver and then cupelled
to yield a precious metal bead. The bead is digested in 0.5 mL
dilute nitric acid in the microwave oven. 0.5 mL concentrated
hydrochloric acid is then added and the bead is further digested in
the microwave at a lower power setting. The digested solution is
cooled, diluted to a total volume of 4 mL with de-mineralized
water, and analyzed by inductively coupled plasma atomic emission
spectrometry against matrix-matched standards.
When gold samples exceed the 10g/t upper
detection limit of Au-ICP/Au-ICP methods, samples are re-assayed
using the following:
Ag-GRA21, Ag-GRA22, Au-GRA21 and Au-GRA22
Precious Metals Gravimetric Analysis Methods Sample Decomposition:
Fire Assay Fusion (FA-FUSAG1, FA-FUSAG2, FA-FUSGV1 and FA-FUSGV2)
Analytical Method: Gravimetric A prepared sample is fused with a
mixture of lead oxide, sodium carbonate, borax, silica and other
reagents in order to produce a lead button. The lead button
containing the precious metals is cupelled to remove the lead. The
remaining gold and silver bead is parted in dilute nitric acid,
annealed and weighed as gold. Silver, if requested, is then
determined by the difference in weights.
Qualified Person
The scientific and technical information in this
news release has been reviewed and approved by Mr. David Gower,
P.Geo., as defined by National Instrument 43-101 of the Canadian
Securities Administrators.
About Halcones
Halcones Precious Metals Corp. is focused on
exploring for and developing gold-silver projects in the Maricunga
Belt, Chile, the premiere gold mining district in South America.
The Company has a team with a strong background of exploration
success in the region.
For further information, please
contact:
Vincent ChenInvestor
Relationsinfo@halconespreciousmetals.comwww.halconespreciousmetals.com
Cautionary Note Regarding
Forward-looking Information
This press release contains “forward-looking
information” within the meaning of applicable Canadian securities
legislation. Forward-looking information includes, without
limitation, regarding the prospectivity of the Project, the
mineralization of the Project, the Company’s exploration program,
the Company’s ability to explore and develop the
Project and the Company’s future plans. Generally, forward-looking
information can be identified by the use of forward-looking
terminology such as “plans”, “expects” or “does not expect”, “is
expected”, “budget”, “scheduled”, “estimates”, “forecasts”,
“intends”, “anticipates” or “does not anticipate”, or “believes”,
or variations of such words and phrases or state that certain
actions, events or results “may”, “could”, “would”, “might” or
“will be taken”, “occur” or “be achieved”. Forward- looking
information is subject to known and unknown risks, uncertainties
and other factors that may cause the actual results, level of
activity, performance or achievements of Halcones, as the case may
be, to be materially different from those expressed or implied by
such forward-looking information, including but not limited to:
general business, economic, competitive, geopolitical and social
uncertainties; the actual results of current exploration
activities; risks associated with operation in foreign
jurisdictions; ability to successfully integrate the purchased
properties; foreign operations risks; and other risks inherent in
the mining industry. Although Halcones has attempted to identify
important factors that could cause actual results to differ
materially from those contained in forward-looking information,
there may be other factors that cause results not to be as
anticipated, estimated or intended. There can be no assurance that
such information will prove to be accurate, as actual results and
future events could differ materially from those anticipated in
such statements. Accordingly, readers should not place undue
reliance on forward-looking information. Halcones does not
undertake to update any forward-looking information, except in
accordance with applicable securities laws.
NEITHER 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.
Halcones Precious Metals (TSXV:HPM)
Historical Stock Chart
Von Dez 2024 bis Jan 2025
Halcones Precious Metals (TSXV:HPM)
Historical Stock Chart
Von Jan 2024 bis Jan 2025