Mirasol Consolidates Large Underexplored Gold – Silver District in Santa Cruz, Argentina
NEWS RELEASE
Suite 910 - 850 West Hastings Street, Vancouver, B.C. Canada, V6C 1E1
Tel: +1 604 602 9989 Fax: +1 604 609 9946 E-mail: [email protected]
www.mirasolresources.com
Mirasol Consolidates Large Underexplored Gold – Silver District
in Santa Cruz, Argentina
VANCOUVER, BC – January 25, 2019 — Mirasol Resources Ltd. (TSX-V: MRZ) (OTCPK: MRZLF) (the “Company”
or “Mirasol” ) is pleased to announce that the Company has signed an option to purchase (OTP) agreement (the
“Agreement”) completing consolidation of the large prospective Sascha – Marcelina Low Sulfidation Epithermal
(LSE) Au-Ag district in Santa Cruz province, Argentina.
Under the terms of the Agreement, Mirasol can acquire 100% of the Marcelina claims from a privately-owned
mining company, by making staged option payments totalling US$3.4 million over 4 years, with US$3.15 million
due on the 4th anniversary. If the OTP is exercised, t he Marcelina claims will be subject to a 1.5% NSR
royalty. There is a minimum US$300,000 exploration spend ing commitment by Mirasol during the first three
years of the option period.
Stephen Nano, President and CEO of Mirasol, state d: “Consolidation of the very prospective Sascha and
Marcelina projects into a large-scale district play has been a long-term objective of Mirasol. This agreement will
allow the multiple underexplored prospects to be systematically explored utilizing the Company’s knowledge of
large-zoned epithermal Au+Ag districts, gained through more than 15 years of successful exploration in Santa
Cruz province.”
Highlights of the Sascha District
• The consolidated Marcelina district has a “footprint” in excess of 65 sq-km, as defined by anomalous Au+Ag
rock chip samples and satellite-based alteration mapping.
• The claims package comprises 30,600 ha of contiguous exploration claims, including the 24,900 ha Sascha
claims, which are 100% owned by Mirasol, and an additional 5,700 ha controlled by Mirasol under the 4-year
OTP agreement.
• The project is centered on the extensive Marcelina “Silica Cap” interpreted to represent the preserved steam
heated alteration and water table silica “blanket”, a feature typical of the near paleosurface level of an LSE
Au+Ag system.
• Multi-kilometre long Au+Ag vein and structural trends , which traverse and outcrop surround ing the
Marcelina Silica Cap, display similarities in areal extent and geological setting to the Cerro Negro Silica Cap,
where GoldCorp operates the “Vein Zone and Bajo Negro” mines in the world class Cerro Negro Au+Ag
Mining District located 100 km to the north of Sascha-Marcelina.
• Rock chip samples from the Sascha-Marcelina district have assays ranging from weakly Au anomalous (10’s
ppb) in the area of the Silica Cap (above the mineralized epithermal interval), up to a peak assay of 160 g/t
Au, (5.14 opt) and 780 g/t Ag (25.07 opt) at the Sascha Main prospect (interpreted top of the high grade
Au+Ag mineralized epithermal interval).
• Initial remodeling of shallow drilling, completed at the 5 km long Sascha Vein trend in 2009 by then Joint
Venture partner Coeur Mining, shows that grade vectors to-depth with interpreted untested Au+Ag “shoots”
of higher-grade mineralization, representing compelling priority targets for drill testing.
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• Other mineralized trends recognized at the project have not been systematically mapped, sampled nor
previously drill tested, suggesting significant potential to define new drill targets along these trends using
current exploration technologies and new deposit models.
• Mirasol is mobilizing a field team to the Marcelina District to be gin a program of systematic surface
exploration to define drill targets. This exploration will initially be focused on the Estancia, Igloo and Sascha
vein trends.
Project History and Ownership
The consolidated district comprises 30,600 ha of contiguous exploration claims. Mirasol staked 16,500 ha of the
claims in 2003, to secure the Sascha Vein Zone (Figure 1, inset 2). At that time the Marcelina claims were held by
competitors. The Mirasol-controlled 5 km-long Sascha Vein Zone was partially drill tested on the western end
while under joint venture to Coeur Mining from 2006 to 2009. Two shallow holes were also drill by Coeur at the
Sasha Sur prospect, into what Mirasol now interprets as the footwall of the structure , which warrants further
testing. Coeur terminated the joint venture in 2009 and returned 100% of the project to Mirasol. On the 23rd of
January 2019, Mirasol signed an OTP for the 5,700 ha Marcelina claims, consolidating the full district under one
company for the first time.
Project Geology and Exploration
Mirasol has recently completed an integrated interpretation of district-scale exploration data sets collected prior
to 2009. Anomalous rock chip Au+Ag assays and Aster satellite alteration anomalies defined a 16.5 x 4.0 km (65
sq. km) “footprint” to the district , showing a large-scale, zoned alteration system characteristic of a large LSE
Au+Ag system (Figure 1). Five, multi-kilometre long, mineralized vein and silicified breccia trends have been
recognized to date across the consolidated district. The trends traverse the Marcelina Silica Cap, or outcrop
through post mineral gravel and basalt cover that surrounds the Silica Cap.
Interpretation of mapped volcanic and sedimentary stratigraphy, Au+Ag and multielement geochemistry and
alteration mineralogy shows that different levels of the epithermal system outcrop across the district, exposing
what are interpreted to be different levels of the mineralized column of an LSE Au+Ag system. These patterns
can be summarized as follows (Figure 2):
Marcelina Silica Cap:
The geologic and geomorphic setting of the Marcelina Silica Cap and related silica structures and veins is
analogous to the Cerro Negro Silica Cap, where Goldcorp is mining plus million ounce Au+Ag resources at Bajo
Negro and Vein Zone deposits, at the Cerro Negro Mine located 100 km to the north of the Sascha – Marcelina
project (Figure 2).
The Marcelina Silica Cap is a three sq. km area of Argillic (kaolinite with minor dickite ± alunite) alteration with
extensive areas of low temperature silica breccia structures and replacement of the host volcanics . The
silicification is interpreted to have been deposited at the top of a hydrothermal system (paleowater table “silica
blanket”) at the time of formation, suggesting that the complete epithermal mineral system maybe preserved at
depth in this area.
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The Silica Cap is cross-cut by large NW and NE oriented silica structures and structural breccias (Pellegrini Trends
1 and 2) , interpreted to represent feeder structures for the silicification . Rock chip sampling of the structures
and breccias returned weakly anomalous Au, averaging 60 ppb and assaying up to 180 ppb Au and up to 11.2
ppm Ag with elevated As, Sb and Hg . The assay results, in conjunction with the interpreted geological setting,
suggest the Pellegrini Trends may represent the upper level of mineralized vein zones, with the potential for high
grade Au+Ag mineralization at depth, and therefore are considered conceptual exploration targets for future drill
testing (Figure 3).
An extensive post mineral gravel “apron” surrounds the immediate area of the Marcelina Silica Cap, concealing
extensions of the alteration system, strike projections of the Au+Ag the silica-breccia structures, and potentially
additional mineralized veins. Systematic mapping and geochemical sampling of the Pellegrini Trends with ground
magnetic and electrical geophysics surveys of the Marcelina Silica Cap and the gravel cover will be used to identify
and refine conceptual targets for later drill testing.
Estancia, Sascha Sur and Igloo trends: These prospect areas are characterized by multi-kilometre long trends of
intermittently outcropping sheeted epithermal veinlet zones up to 20 m wide and locally developed breccia
pipes, with multiphase hydrothermal brecciation (Figure 4). The host volcanics are altered to an intermediate
argillic assemblage of illite-smectite clays. Initial rock chip sampling of these trends averages approximately 150
ppb Au with peak assays up to 1.62 g/t Au and up to 158 g/t Ag.
The alteration assemblage, assay results and silica textures seen at these prospects, are consistent with the
interpretation that these trends may represent the top of the mineralized interval in an LSE system. The
anomalous Au+Ag assays potentially represent geochemical leakage from concealed higher-grade precious metal
mineralization at shallow (100 – 200m) depths.
The host rocks at the current outcrop level of the Estancia, Sascha Sur and Igloo trends, are ash and crystal tuffs
of the uppe r middle Jurassic Matilda formation. These volcanics are poor host rocks for large fissure vein
formation. However, Mirasol’s stratigraphic mapping at the Marcelina project shows that more permissive host
rocks for fissure vein formation, including welded ignimbrit e flows of the middle Jurassic Chon Aike formation ,
are present in the stratigraphy underlying these prospects. Mirasol will use a combination of detailed geological
– structural mapping, selective geochemical sampling, alteration vectoring studies and ele ctrical geophysics to
refine targets for drill testing.
The Estancia, Sascha Sur and Igloo trends represent priority drill targets for potential high -grade Au+Ag
mineralization and will be the initial focus of surface exploration.
Sascha Main: Previous surface mapping and rock chip sampling (see Sascha Gold-Silver Project 43-101 Technical
Report, 2004 and news release February 21, 2006) of the Sascha Main prospect identified outcrop expressions
of a series of mineralized “shoots” hosting high grade Au+Ag mineralization . Rock chip assays of this material
ranged up to 160 g/t Au, and 780 g/t Ag, with precious metal mineralization reporting to chalcedony – adularia
colloform banded pulses hosting fine bands of sulfides and native Au (“ginguro” phases).
Previous JV partner drilling at the Sascha vein zone (see news release September 5, 2007) included 19 diamond
drill holes that partially tested the vein zone to a maximum depth of 200 m. Drilling intersected narrow zones of
Au+Ag mineralization including a best interval of 1.55 m at 8.92 g/t Au and 27.7 g/t Ag (Hole DDS-02) but did not
intersect the ging uro phases with native Au evident at surface . Mirasol’s remodeling of the Sascha Main
www.mirasolresources.com
exploration data suggests that the drilling may not have tested the targets optimally, possibly missing the “tops”
of plunging high grade shoots that could potentially to extend to depth. These “shoot tops” are priority targets
for drill testing at the Sascha Main prospect.
Stephen Nano, President and CEO of Mirasol, has approved the technical content of this news release. Mr Nano
is a Ch arter Professional geologist and Fello w of the Australasian Institut e of Mining and Metallurgy (CP and
FAusIMM) and is a Qualified Person under NI 43 -101.
For further information, please contact
Stephen Nano
CEO and President
or
Jonathan Rosset
VP Corporate Development
Tel: +1 (604) 602-9989
Email: [email protected]
Website: www.mirasolresources.com
Additional Explanatory Notes:
* AuEq60 is the sum of the value of gold and silver in a given interval represented as a gold equivalent g/t value calculated via the
formula: Au assay in g/t + (silver assay in g/t ÷ 60)
Quality Assurance/Quality Control of the Sascha exploration program:
All exploration on the project was supervised by Mirasol CEO Stephen C. Nano, who is the Qualified Person under NI 43-101.
Mirasol applies industry standard exploration sampling methodologies and techniques. All geochemical soil, stream, rock and drill samples
are collected under the supervision of the company’s geologists in accordance with industry practice. Geochemical assays are obtained
and reported under a quality assurance and quality control (QA/QC) program. Samples are dispatched to an ISO 9001:2008 accredited
laboratory in Argentina for analysis. Assay results from surface rock, channel, trench, and drill core samples may be higher, lower or similar
to results obtained from surface samples due to surficial oxidation and enrichment processes or due to natural geological grade variations
in the primary mineralization.
Forward Looking Statements: The information in this news release contains forward looking statements that are subject to a number of
known and unknown risks, uncertainties and other factors that may cause actual results to differ materially from those anticipated in our
forward-looking statements. Factors that could cause such differences include: changes in world commodity markets, equity markets,
costs and supply of materials relevant to the mining industry, change in government and changes to regulations affecting the mining
industry. Forward-looking statements in this release include statements regarding future exploration programs, operation plans,
geological interpretations, mineral tenure issues and mineral recovery processes. Although we believe the expectations reflected in our
forward-looking statements are reasonable, results may vary, and we cannot guarantee future results, levels of activity, performance or
achievements. Mirasol disclaims any obligations to update or revise any forward-looking statements whether as a result of new
information, future events or otherwise, except as may be required by applicable law.
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.
Suite 910 - 850 West Hastings Street, Vancouver, B.C. Canada, V6C 1E1
Tel: +1 604 602 9989 Fax: +1 604 609 9946 E-mail: [email protected]
1,000m
Figure 1: Marcelina Gold-Silver District - Multiple Mineralized Au-Ag Epithermal Vein Trends. January 2019
Post min
basalt cover
Post min
basalt cover
Post min
gravel
apron
Undifferentiated
cover
Salt pan
Salt
pan
Salt pan
Undifferentiated
cover
Post min
gravel
apron
Marcelina
Claims
Sascha claims
Sascha
claims
65 km
2
Au
-
Ag district
Claims boundary
Jurassic
Volcanics
Post min
basalt cover
Jurassic
Volcanics
Jurassic
Volcanics
Jurassic
Volcanics
Santa
Cruz
Province
Argentina
Chile
50km
Sascha
-
Marcelina
claims
Cerro Negro
Cerro
M
orro
Mina Martha
Manatial
Espejo
Jurassic
volcanics
Cerro
Vanguardia
2,500m5,000m
Rock Chip Assays - ppm
By Gold Equivalent (Au + Ag / 60)
1.00 to 168.00
0.25 to 1.00
0.10 to 0.25
0.05 to 0.10
0.00 to 0.05
Below Detection
0.05 to 0.10
100% Kaolinite
100% Illite
Kaolinite-Illite
Mixture
ASTER Alteration
Intensity
Inset 1 Inset 2 Inset 3
Marcelina
Silica Cap
Figure 2: Marcelina Gold-Silver District - Comparison to Goldcorp’s Cerro Negro Operation. January 2019
Cerro Negro
Reserves and
Resources
Baja Negro
Mariana
Vein Zone
Cerro Negro
Silica Cap
Mariana Norte
San Marcos
Eureka
Proven & Probable Reserves
5.02 Moz Au @ 8.75g/t
35.20 Moz Ag @ 61.4 g/t
*June 2018
Goldcorp Cerro Negro
Gold – Silver Mining District
Mirasol Resources Marcelina District
Exploration Project
1 Goldcorp. 2015. Cerro Negro Operations Santa Cruz Province, Argentina NI 43-
101 Technical Report.
2 Goldcorp. October 24, 2018. Goldcorp Reports 2018 Reserve and
Resource Estimates and Provides Exploration Update.
Marcelina
Silica Cap
2,500 m
2,500 m
Figure 3: Marcelina Gold-Silver District - Low Sulfidation Epithermal Model. January 2019
B.
A.
C.
D.
B.
Pellegrini Trends
–
hematite
–
silica breccia in structural feeders
cross cut water table silica
A.
Marcelina Silica Cap: Opal and Chalcedonic in structural feeders and
silica replacement of the host Volcanic at the paleowater table
D. Sascha Vein Zone
–
Colloform
–
Crustiform
quartz
-
adularia with
“
Ginguro
” bands with visible electrum
C. Estancia Trend
–
Vein top
breccias and sheeted veinlets
with colloform
–
crustiform
matrix and smectite > illite
altered volcanic wall rock
Sascha vein peak rock assays 160 g/t Au 780 g/t Ag
Vehicle for scale
Sascha Sur/Estancia/
Igloo Trends
5 – 1000 ppb Au
1 – 10 ppm Ag
Pellegrini Trends
Silica Replacement
BDL – 10 ppb Au
BDL – 1.5 ppm Ag
Feeder Structures
BDL – 177 ppb Au
BDL – 2 ppm Ag
Sascha Main
Avg. 4.21 ppm Au
Avg. 22.70 ppm Ag
Max 160.0 ppm Au
Max 780 .0 ppm Ag
Primary Structure
Hanging wall
stringer zone
Footwall
stringer zone
Capping
Basalt
Flows
Jurassic Volcanics
350 m long up to 25 m wide zone
of high level epithermal veining.
Systematic rock chip sampling required
High level vein top breccia
-
assays pending
New zone of epithermal
veining
–
assays pending
C.
B.
A.
A & B
C
100% Kaolinite
100% Illite
Kaolinite-Illite
Mixture
ASTER Alteration
Intensity
Marcelina
Claims
Sascha claims
Sascha
claims
500m
Post Min
Gravel
Apron
Post Min
Gravel
Figure 4: Marcelina Gold-Silver District – Estancia Trend Epithermal Veining. January 2019
Jurassic Volcanics
B.
Capping
Basalt
Flows
Capping
Basalt
Flows
Post Min
Gravel
Zone of new veining
Systematic rock chip
sampling required