Highlights
- Drilling results confirmed presence of gold mineralization
hosted within silicified diatreme breccias within a 1.5km trend
along the eastern portion of the Lourdes project area
- The drill hole intercepts to date suggest the eastern target
areas of Cascada, Paccha Huayco and Chucllani are one large
contiguous system favorable for gold mineralization
- Lourdes Phase II drilling will focus on step-out drilling to
locate the Chucllani–Paccha Huayco structural feeder, test the
Cascada Diatreme, and follow up on targets identified from
interpretation of Phase I drill data
- 2021 Plans include Lourdes Phase II drillling, additional
target generation at Pacaska Gold–Copper Project while awaiting
drill permits, and advancing the Keyla Gold Project to drill ready
status
- Year-end 2020 treasury of of C$5.5M fully funds 2021 work programs
VANCOUVER, BC, Jan. 26, 2021 /CNW/ - Pucara Gold
Ltd. ("Pucara Gold", "Pucara" or the
"Company") (TSXV: TORO) announces that 25 holes totalling
3,955m of drilling (see figure 1 and
appendix 1) were successfully completed on budget and safely at the
Lourdes Gold Project in Peru.
Drilling results confirmed the presence of gold mineralization
hosted within silicified diatreme breccias within a 1.5km trend
along the eastern portion of the Lourdes project area. Five of the nine
target areas were tested with follow up drilling planned during
Phase II.
The most significant gold intercepts (see table 1) obtained from
the Chucllani area included 0.24 g/t gold over 18m in drill hole LOU011, 0.24 g/t gold over
21m in nearby drill hole LOU013 (see
figure 2) and 0.47g/t gold over 4.9m
in drill hole LOU019. These mineralized intercepts appear
stratiform and are believed to represent the distal portion of the
Paccha Huayco diatreme, leaving a large portion of the inferred
structural feeder to be tested in the Phase II campaign.
Drill holes in the North Diatreme and the northern portion of
the Jellopata diatreme target areas encountered substantial
thicknesses of favorable silicic alteration and confirmed the
target concept. Gold mineralization was not encountered. Drill hole
intercepts suggest remaining potential to the south due to an
inferred vector toward coarse diatreme breccias indicative of the
vent source, the increased presence of massive to vuggy silica with
depth, limonite contents, and anomalous gold in surface
sampling.
Ken Balleweg, VP Exploration,
"Our initial drill program at Lourdes was testing an area of approximately
six square kilometers and will require additional holes to test the
full potential of the targets. This first subsurface data has
allowed us to focus in on the most promising area of the greater
Paccha Huayco complex. The Chucllani intercepts provide an
encouraging vector toward the structural feeder that has the
highest probability of hosting an economic gold deposit."
Steve Zuker, CEO." We are
encouraged by the results of the first ever drill program at
Lourdes. Our drill program gave us
critical information in the third dimension, assisting us to target
the best host rocks, alteration, and structural setting for gold
deposition. We will use this new information to target drilling for
Phase II and to prioritize numerous attractive, but previously less
understood, target areas. We are well financed to continue with
Phase II drilling at Lourdes and
initiate the first ever drill campaign at our Pacaska Gold-Copper
Project."
Discussion of Phase I Results
Chucllani Zone
Seven holes were drilled into the target area totalling
856m. The most significant gold
intercepts include 0.24 g/t gold over 18m in drill hole LOU011 and 0.24 g/t gold over
21m in drill hole LOU013.
Chucllani has strong similarities of mineralization and
alteration to the Apumayo gold deposits being mined 14km to the
south. The primary drill target consisted of a more than
200m long northeast-trending zone of
granular silica alteration with outcropping gold mineralization up
to 0.64 g/t Au. Drilling indicates that the gold zone is
stratiform, occurring in the basal portion of a zone of granular to
massive silica extending laterally outward from the Paccha Huayco
diatreme and outcropping 150m south
of the drill collars. While low-grade, the zone is comparable to
granular-silica hosted ore-grade mineralization at the Apumayo
Mine.
The Chucillani intercepts are most likely the distal portion of
a structurally controlled gold zone located to the northwest toward
the Paccha Huayco diatreme and warrants additional step-out
drilling to be included in Phase II.
Drilling indicates that the Chucllani zone exhibits moderate to
strong multi-element geochemistry with elevated pathfinder
elements: arsenic, bismuth, barium, and mercury.
Paccha Huayco Complex
Core hole (LOU012) into the Paccha Huayco target confirmed the
diatreme concept, transecting 230m of
strongly silicified multi-stage diatreme breccias.
Multiple stages of cross-cutting hydrothermal breccias are
present, as well as late-stage cross-cutting silica veinlets
similar to those carrying gold at the Apumayo Mine. Anomalous gold
concentrations were encountered at depth and appear to be
correlative with Chucllani intercepts. The hole ended in strongly
altered andesite host rock, indicating that the hole is not located
in the central diatreme vent area and the target therefore requires
additional exploration drilling.
Jellopata Diatreme Target
Eight holes were drilled into the northern 600m of the 1.2km long Jellopata diatreme
resistivity anomaly and targeted the inferred central diatreme
feeder. Thick 100m to 229m plus intercepts of highly oxidized granular
to massive silica alteration were encountered that are anomalous in
molybdenum but lack anomalous gold concentrations.
One Jellopata drill hole (LOU003) appears to have penetrated
close to the inferred diatreme feeder, with the others transecting
altered lateral and distal stratiform diatreme fill sediments.
Drill hole LOU003 had the thickest silica interval encountered of
229m, and the hole was lost in
favorable silicic alteration in a fault zone at 246m. The hole showed transition to more
favorable vuggy and massive silica with higher limonite content at
depth.
The character of the drill hole lithologies suggest remaining
potential to the south due to the presence of coarser diatreme fill
breccias, increased massive to vuggy silica with depth, higher
limonite contents and more gold in surface sampling.
Ayani Vent Target
Four holes were drilled into the Ayani target, a structurally
controlled zone located at the extreme northeastern portion of the
Lourdes system. Drill holes
encountered the strongest trace element geochemical signature of
the program and weakly anomalous gold. Alteration indicative of the
upper barren portion of the hydrothermal system was encountered;
follow-up drilling will test the deeper portions of the zone.
North Diatreme Zone
Two holes were drilled into the North Zone, located at the
extreme northern end of the project area with outcropping
northeast-trending silicified hydrothermal breccias, granular
silica breccias, and silicified limonitic matrix breccias highly
anomalous in pathfinder elements. Both holes encountered strongly
anomalous molybdenum and weakly anomalous gold concentrations.
Cascada Diatreme Target
The Cascada target, containing some of the most continuous
outcropping gold mineralization, was not tested during the Phase I
program due to difficult access. Plans are to test the target at
the start of the Phase II program.
Drill hole intercepts to date suggest that the Cascada–Paccha
Huayco–Chucllani area is a larger continuous system and the most
favorable for gold mineralization.
Table 1. Summary of assay results and significant gold
intercepts.
Drill
Hole
|
Target
Area
|
Drill
Method1
|
Azimuth°
|
Dip°
|
Total
Depth (m)
|
From
(m)
|
To
(m)
|
Interval
1 (m)
|
Gold
(g/t)
|
LOU008
|
Chucllani
|
RC
|
320
|
-45
|
126
|
0.0
|
3
|
3
|
0.18
|
LOU009
|
Chucllani
|
RC
|
320
|
-55
|
159
|
79.5
|
85.5
|
6
|
0.17
|
LOU011
|
Chucllani
Paccha Huayco
|
RC
|
270
|
-50
|
192
|
84
|
102
|
18
|
0.24
|
LOU012
|
Paccha
Huayco
|
CORE
|
270
|
-70
|
265.7
|
180.6
191.2
|
183.6
201
|
3
9.8
|
0.12
0.11
|
LOU013
|
Chucllani
|
RC
|
170
|
-50
|
114
|
42
|
63
|
21
|
0.24
|
LOU019
|
Chucllani
Paccha Huayco
|
CORE
|
270
|
-75
|
133.2
|
78.7
|
84.6
|
4.9
|
0.47
|
1
Intersections presented herein may not necessarily represent true
width of mineralization, are interpreted to be approximately
representative due to the stratiform nature of the zone, indicated
dip angle from geophysics, and hole inclination.
|
Phase II Plans
The Phase II drilling program is planned to recommence after the
end of the rainy season in April. Evaluation of the drilling data
will continue over the next months and will be integrated with into
the existing exploration data to improve targeting for follow-up
drilling. Phase II drilling will focus on step-out drilling to
locate the Chucllani–Paccha Huayco structural feeder, testing the
Cascada Diatreme, and following up on other targets identified from
the Phase I drill campaign.
Quality Assurance
Pucara has a Quality Assurance and Quality Control ("QA/QC")
program for all of its exploration projects which conforms to
industry best practices. Samples are sent to ALS PERU SA, an ISO/IEC 17025:2017 accredited
laboratory, in Lima, Peru for
analysis. Analytical method is a 30-gram fire assay with atomic
adsorption finish. Strict sampling and QA/QC protocol are followed,
including the insertion of standards, blanks, and duplicates on a
routine basis. Results of these QC samples are tracked and failures
are re-analyzed. Sample intervals are usually 1.5m. All exploration diamond drill cores are
split in half by core sawing and sampled at appropriate intervals
for assay. The remaining core, coarse reject and pulps are stored
on-site in a secure location. Composites presented in the assay
results table include intervals at greater than 0.1 g/t Au over a
1.5m minimum width.
About Lourdes Gold Project
The wholly-owned Lourdes Gold Project is a fully-permitted, high
sulfidation epithermal precious metal project, which lies at the
intersection of two regional mineralized trends with neighboring
high sulfidation prospects and a producing mine. Pucara has
identified a complex of nested diatremes, vent breccias, and
breccia bodies at Lourdes that are
similar in size (km2) and associated alteration to the
high sulfidation epithermal gold deposits at Yanacocha and Pierina
in northern Peru, and the Mulatos
district of Mexico. The 2,576
hectare-property is approximately 400 kilometres southeast of
Lima and is easily accessible by a
paved, single-lane road originating in the town of Puquio, 155
kilometres east of the Pan American Highway.
About Pacaska Gold — Copper Project
The Pacaska Gold-Copper Project consists of a highly prospective
and contiguous area of 7,650 hectares over nine concessions, wholly
owned by Pucara Gold. Pacaska is a high sulfidation epithermal
precious metals project with a possible copper porphyry system at
depth. The alteration system contains anomalous, outcropping
concentrations of gold with values in rock of up to 17 g/t and
anomalous copper in rock of up to 11%. Pacaska is easily accessible
by a paved, single lane road originating at the Pan American
Highway in the town of Palpa 90 kilometres southwest of
Pacaska.
The Company is currently permitting the Pacaska project for
drill testing, after completion of a large IP survey, which
identified resistivity anomalies extending to depth correlative
with the gold-bearing breccias, as well as a large broad
chargeability anomaly suggestive of a porphyry copper system.
Multiple drill targets have been selected. The Company expects to
inform the market about its 2021 work program at Pacaska in a
forthcoming corporate update.
About Pucara Gold
Pucara Gold is a well-financed junior exploration company
focused on the discovery and advancement of economic precious
metals deposits in resource-rich Peru. Pucara has a portfolio approach to
project acquisition and controls nine precious and base metal
projects, located in Peru. Pucara
is advancing six projects while the remaining three are under
option agreements with strategic partners. Pucara plans to grow
through discoveries, strategic relationships, and grassroots
exploration. For more information, please visit Pucara Gold's
YouTube channel.
Qualified Person
The Lourdes exploration
programs are conducted under the supervision of Ken Balleweg, B.Sc. Geological Engineering,
M.Sc. Geology, Registered Professional Geologist, Vice President of
Exploration, a Qualified Person as defined by National Instrument
43-101 of the Canadian Securities Administrators.
Cautionary Statements
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. This news release includes
forward-looking statements that are subject to risks and
uncertainties. All statements within, other than statements of
historical fact, are to be considered forward looking. Although the
Company believes the expectations expressed in such forward-looking
statements are based on reasonable assumptions, such statements are
not guarantees of future performance and actual results or
developments may differ materially from those in forward-looking
statements. Factors that could cause actual results to differ
materially from those in forward-looking statements include market
prices, exploitation and exploration successes, the impact of the
COVID-19 pandemic on the worldwide economy, continued availability
of capital and financing, and general economic, market or business
conditions and regulatory and administrative approvals, processes
and filing requirements. There can be no assurances that such
statements will prove accurate and, therefore, readers are advised
to rely on their own evaluation of such uncertainties. We do not
assume any obligation to update any forward-looking
statements.
Appendix 1: Phase I Drill Collars
Drill
Hole
|
Target
Area
1
|
Drill
Method
|
UTM
East
|
UTM
North
|
Azimuth°
|
Dip°
|
Total
Depth (m)
|
Note
2
|
LOU001
|
Jellopata
|
RC
|
617,740
|
8,364,300
|
270
|
-65
|
252
|
NS
|
LOU002
|
Jellopata
|
RC
|
617,750
|
8,364,100
|
270
|
-65
|
201
|
NS
|
LOU003
|
Jellopata
|
RC
|
617,750
|
8,364,100
|
090
|
-65
|
246
|
NS
|
LOU004
|
Jellopata
|
RC
|
617,700
|
8,363,900
|
270
|
-75
|
180
|
NS
|
LOU005
|
Jellopata
|
RC
|
617,750
|
8,363,700
|
270
|
-70
|
216
|
NS
|
LOU006
|
Jellopata
|
RC
|
617,550
|
8,364,300
|
0
|
-90
|
210
|
NS
|
LOU007
|
Jellopata
|
CORE
|
617,700
|
8,363,900
|
090
|
-65
|
170
|
NS
|
LOU008
|
Chucllani
|
RC
|
619,310
|
8,363,725
|
320
|
-45
|
126
|
See Table
1
|
LOU009
|
Chucllani
|
RC
|
619,250
|
8,363,900
|
320
|
-55
|
159
|
See Table
1
|
LOU010
|
Jellopata
|
CORE
|
617,750
|
8,363,700
|
090
|
-70
|
148.2
|
NS
|
LOU011
|
Chucllani
Paccha
Huayco
|
RC
|
619,250
|
8,363,900
|
270
|
-50
|
192
|
See Table
1
|
LOU012
|
Paccha
Huayco
|
CORE
|
619,095
|
8,364,115
|
270
|
-70
|
265.7
|
See Table
1
|
LOU013
|
Chucllani
|
RC
|
619,250
|
8,363,900
|
170
|
-50
|
114
|
See Table
1
|
LOU014
|
Ayani
|
RC
|
619,775
|
8,364,500
|
300
|
-45
|
63
|
NS
|
LOU015
|
Ayani
|
RC
|
619,470
|
8,364,500
|
300
|
-55
|
75
|
NS
|
LOU016
|
Ayani
|
RC
|
619,850
|
8,364,570
|
300
|
-50
|
114
|
NS
|
LOU017
|
Chucllani
|
RC
|
619,625
|
8,364,000
|
270
|
-53
|
60
|
NS
|
LOU018
|
Chucllani
|
RC
|
619,625
|
8,364,000
|
220
|
-55
|
72
|
NS
|
LOU019
|
Chucllani
Paccha
Huayco
|
CORE
|
619,185
|
8,364,100
|
270
|
-75
|
133.2
|
See Table
1
|
LOU020
|
Ayani
|
RC
|
619,635
|
8,364,510
|
325
|
-55
|
126
|
NS
|
LOU021
|
Paccha Huayco
East
|
RC
|
618,870
|
8,364,100
|
270
|
-70
|
154.5
|
NS
|
LOU022
|
Paccha Huayco
East
|
RC
|
618,870
|
8,364,100
|
140
|
-60
|
177
|
NS
|
LOU023
|
North
|
CORE
|
617,500
|
8,365,660
|
350
|
-50
|
144.7
|
NS
|
LOU024
|
North SE
Ext
|
CORE
|
617,640
|
8,365,500
|
0
|
-90
|
151.8
|
NS
|
LOU025
|
Paccha Huayco
East
|
RC
|
618,750
|
8,363,900
|
270
|
-85
|
204
|
NS
|
1 See
figure 1 for location of Target areas.
2 NS – No significant mineralization.
|
SOURCE Pucara Gold Ltd.