Cornerstone Capital Resources Inc. (“Cornerstone” or “the
Company”) (TSXV:CGP) (Frankfurt:GWN) (Berlin:GWN)
(OTC:CTNXF) is pleased to announce the following update on
the exploration results at the Espejo project located within the
Cornerstone Ecuador S.A. (“CESA”) - ENAMI EP strategic exploration
alliance (the “ENAMI-CESA SEA”) in Northern Ecuador (See “About the
ENAMI EP - Cornerstone Strategic Exploration Alliance (SEA)”,
below), in which CESA has the option to earn up to an 84% interest.
Figures related to this news release can be seen
in PDF format by accessing the version of this release on the
Company’s website (www.cornerstoneresources.com) or by clicking on
the link below:
https://cornerstoneresources.com/site/assets/files/5859/nr22-15figures.pdf.
HIGHLIGHTS:
- Strong rock sampling
results confirm the potential of the high priority porphyry Cu-Au
and Cu-Mo targets previously identified within three main target
areas
- Age dating, alteration and
mineralization patterns confirm the presence of Cascabel-type
porphyry Cu-Au and Llurimagua-type porphyry Cu-Mo mineralized
systems
Cornerstone VP Exploration, Yvan Crepeau,
said:
“We were encouraged early on when prospecting
the Espejo project, mapping prospective geology, porphyry-style
alteration and mineralization and delineating kilometric size soil
anomalies. Follow up on these anomalies is even more encouraging.
Copper, gold and molybdenum assay results from rock sampling are
highly anomalous and consistent over several hundreds of metres on
each target. And there is an excellent correlation between geology,
geophysics and geochem. We now have all the elements in hand to
define individual Phase 1 drilling programs on these 3
targets.”
We would like to thank Cornerstone’s exploration
and support teams, local communities and authorities, and ENAMI’s
management and technical staff for their assistance and support
since the beginning of the programs.”
FURTHER INFORMATION:
Cornerstone Ecuador SA (“CESA”), a wholly owned
subsidiary of Cornerstone Capital Resources Inc. (TSXV: CGP), has
outlined several high priority porphyry Cu-Au (Mo) Cu-Mo (Au)
exploration target areas on its Espejo project located in El Carchi
province, in northern Ecuador. See News Releases 20-05 (February
27, 2022) and 21-05 (March 4, 2022) and the location map in
Figure 1.
Since our last update, soil sampling grids
covering the full extension of the previously defined geochemical
anomalies, detailed spectrometry and geological mapping and
extensive rock chip channel sampling were carried out to support
geological modeling and refine drill target proposals. To date,
2401 rock samples, 4446 soil samples and 665 stream sediment
samples have been collected on the Espejo project. The regional
U/Pb age dating and detailed geochemical (major, trace and REE
elements) program was completed helping to define and characterize
various intrusive complexes, source of porphyry style
mineralization in this part of NW Ecuador. Preliminary data
indicate an age varying from 8.9 to 7.7 My (million years) at
Espejo for most intrusives associated to Cu-Mo mineralization,
similar in age to that found at the Llurimagua project (Schutte
2010), except in one area where geological mapping, spectrometry
and geochemical work were initially suggestive of a Cascabel-type
of environment and mineralization (Figure 1). Age
dating at Anomaly #3 confirmed this hypothesis.
Recent work on this property indicates a strong
structural regional NE-SW and more local NW-SE geological and
mineralization controls. Multiphase intrusive complexes and related
mineralization are usually located at (or close to) the junction of
these two structural trends.
Anomaly ESP # 1 – Porphyry Cu-Mo (Au)
target
The ESP #1 area is underlain by a series of
sandstones and shales interbedded with volcanic tuff units of
andesitic composition. A mylonite zone is developed at the junction
of a NE oriented regional structure and NW-SE conjugated local
structures. Small stocks of quartz diorite are emplaced along
and/or parallel to stratification and along NE-SW oriented faults.
There is a mild to moderate potassium alteration in the intrusives
and milonite with the presence of quartz (Qz) – pyrite (Py) ±
chalcopyrite (Cpy) ± molybdenite (Mo) veins of NNW – SSE direction.
Several samples were collected for age dating using U-Pb isotopes.
Mineralized intrusives are of Miocene age, varying from 10.9 My to
11.9 My (Figure 2).
This prospective area was discovered through
regional sampling and prospecting programs. The NW-SE oriented
in-soil anomaly is 1800m long by 700 to 1200m wide and open to the
NW where porphyry style mineralization and veining was found in the
creeks some 500m in this direction. The soil copper, molybdenum and
gold anomalies are confirmed by strong rock chip channel assay
results (Figure 2).
3D magnetic inversion modeling was carried out
on this target. Data shows strong and extensive magnetic bodies
below the Cu-Mo (Au) anomaly down to > 1500m below surface and
associated to an intrusive complex centered right below the
anomalous zone. The initially proposed Phase 1 drilling program is
now being reviewed and refined, incorporating newly generated
information.
Anomaly ESP # 2 – Porphyry Cu-Mo (Au)
target
The geological basement of the ESP #2 anomaly is
composed of andesitic lava flows and tuffs which have been intruded
by several quartz diorite stocks and a series of andesitic to
dacitic porphyries. At least four phases of dacite porphyries were
identified. Most representative hydrothermal alteration consists of
mild to moderate potassic alteration and the presence of B-type
Qz-Py-Cpy veins which host the most significant part of the
mineralization. NW-SE trending faults and structures appear to
control the presence of the intrusives and sub-parallel veins. As
for anomaly #1 above, mineralized intrusives are of Miocene age,
varying from 7.7 My to 8.1 My (Figure 3).
A large (1100m by 800m), NW-SE elongated, and
Cu-Mo-Au coincident in-soil anomaly was prospected and rock
sampled. Systematic chip channel sampling yielded strong and
consistent highly anomalous assay results over most part of the
soil anomaly as shown on Figure 3. Mineralization
is associated to potassic and phyllic altered intrusives and
volcanic host rocks.
Similar magnetic data processing and modeling
was performed on the ESP #2 anomaly showing the presence of several
magnetic bodies at depth. The conceptual Phase 1 drilling program
for testing the surface (geology and geochem) and sub-surface
(magnetic) anomalies previously designed is now being refined
incorporating recent geological mapping and rock sampling
information.
Anomaly ESP #3 – Porphyry Cu-Au (Mo)
target
Although geology, alteration and controls of
mineralization present at Anomaly #3 are similar to Anomalies #1
and #2, geological age and metals distribution are different.
Similar equigranular to sub-porphyritic stock of dioritic
composition intrude a basement formed of sedimentary and
volcanogenic sediments. A total of four intrusive phases were
identified. These stocks show a mild to moderate potassic
alteration and Cu-Au (Mo) mineralization associated M-type
(Qz-Magnetite-Cpy), B-type (Qz-Py-Cpy) and D-type (Qz-Py-sericite)
veins. NNW – SSE structures appear to control the presence of
diorite bodies and other porphyries. Several samples were collected
for age dating. Most of them were zircon-poor but one sample
indicates an older 31.4 My age, Lower Oligocene, close to Cascabel
age. Alteration and mineralization patterns are also similar to
Cascabel.
The large (1600m by 1200m), coincident Cu-Au-Mo
anomalous zone is also NNW-SSE oriented (Figure
4). Assay results from channel rock chip sampling indicate
a very strong correlation with the soil anomaly and between these 3
elements. Two Cu-Mo centers appear to be developed in the NW and in
the SE parts of the larger anomalous area, with higher gold content
in the SE part.
About the ENAMI EP - Cornerstone Strategic Exploration
Alliance (SEA)
On June 14, 2016, Cornerstone announced that its
Ecuadorean subsidiary, Cornerstone Ecuador S.A. (“CESA”), had
signed a Spanish language Agreement, or Acuerdo de Colaboración e
Inversión para el Desarrollo Conjunto de Proyectos de Exploración
Minera (the “Agreement”) with Ecuador’s State Mining Company,
Empresa Nacional Minera Empresa Pública (“ENAMI EP”), replacing a
letter of intent announced April 14, 2015, and creating a structure
to jointly prospect and explore for mineral deposits in Ecuador
(the “ENAMI-CESA Strategic Exploration Alliance” or “ENAMI-CESA
SEA”).
The Espejo block of four concessions was
identified and ranked by Cornerstone in 2015-2016 as highly
prospective after an exhaustive analysis of public and private
information available at the time, reserved by CESA after the
opening of the cadastral map and then the reservations were
transferred to ENAMI for inclusion in the SEA.
On March 6, 2017, Cornerstone announced that
ENAMI EP had been granted a number of mineral concessions in
Imbabura and Carchi provinces in the same general area as the
Cascabel (SolGold/Cornerstone) and Llurimagua (Codelco/Enami)
concessions, for exploration by the ENAMI-CESA SEA.
For more information about the ENAMI-CESA SEA,
please see Cornerstone news release 16-12 dated June 14, 2016
https://cornerstoneresources.com/news-releases/16-12-cornerstone-signs-definitive-joint-exploration-agreement-with-ecuadors-state-mining-company-enami-ep/.
About Cornerstone
Cornerstone Capital Resources Inc. is a mineral
exploration company with a diversified portfolio of projects in
Ecuador and Chile, including the Cascabel gold-enriched copper
porphyry joint venture in northwest Ecuador. Cornerstone has a
20.8% direct and indirect interest in Cascabel comprised of (i) a
direct 15% interest in the project financed through to completion
of a feasibility study and repayable at Libor plus 2% out of 90% of
its share of the earnings or dividends from an operation at
Cascabel, plus (ii) an indirect interest comprised of 6.85% of the
shares of joint venture partner and project operator SolGold Plc.
Exploraciones Novomining S.A. (“ENSA”), an Ecuadoran company owned
by SolGold and Cornerstone, holds 100% of the Cascabel concession.
Subject to the satisfaction of certain conditions, including
SolGold’s fully funding the project through to feasibility, SolGold
Plc will own 85% of the equity of ENSA and Cornerstone will own the
remaining 15% of ENSA.
Qualified Person
Yvan Crepeau, MBA, P.Geo., Cornerstone’s Vice
President, Exploration and a qualified person in accordance with
National Instrument 43-101, is responsible for supervising the
exploration program at the Espejo project for Cornerstone and has
reviewed and approved the information contained in this news
release.
Sampling and assaying
CESA uses a fire assay gold technique for Au
assays (FAS-111) and a four acid multi element technique (IMS-230)
for a suite of 48 elements. FAS-111 involves Au by Fire Assay on a
30-gram aliquot, fusion and atomic absorption spectroscopy (AAS) at
trace levels. IMS-20 is considered a near total 4 acid technique
using a 20g aliquot followed by multi-element analysis by
ICP-AES/MS at ultra-trace levels. This analysis technique is
considered suitable for this style of mineralization.
Standards, blanks and duplicates are inserted
~1/25 samples. The values of the standards range from low to high
grade and are considered appropriate to monitor performance of
values near cut-off and near the mean grade of the deposit. The
check sampling results are monitored and performance issues are
communicated to the laboratory if necessary.
Sample security was managed through sealed
individual samples and sealed bags of multiple samples for secure
delivery to the laboratory by permanent staff of the joint-venture.
MS Analytical is an internationally accredited laboratory that has
all its internal procedures heavily scrutinized in order to
maintain their accreditation. MS Analytical is accredited to
ISO/IEC 17025 2005 Accredited Methods.
CESA’s sampling techniques and data have been
audited multiple times by independent mining consultants during
various project assessments. These audits have concluded that the
sampling techniques and data management are to industry standards.
All historical data has been validated to the best degree possible
and migrated into a database.
Rock samples are collected by CESA’s personnel,
placed in plastic bags, labeled and sealed, and stored in a secure
place until delivery by CESA employees to the LAC y Asociados ISO
9001-2008 certified sample preparation facility in Cuenca,
Ecuador.
Rock samples are prepared crushing to 70%
passing 2 mm (10 mesh), splitting 250 g and pulverizing to 85%
passing 75 microns (200 mesh) (MSA code PRP-910). Prepared samples
are then shipped to MS Analytical Services (MSA), an ISO 9001-2008
laboratory in Langley, BC, Canada, where samples are assayed for a
multi-element suite (MSA code IMS-136, 15.0 g split, Aqua Regia
digestion, ICP-AES/MS finish) and gold by Fire Assay (MSA code
FAS-111, 30 g fusion, AAS finish). Over limit results for Cu
(>1%) are systematically re-assayed (MSA code ICF-6Cu, 0.2 g,
4-acid digestion, ICP-AES finish). Gold is assayed using a 30 g
split, Fire Assay (FA) and AAS finish (MSA code FAS 111). Over
limit results for Au (>10 g/t) are systematically re-assayed
(MSA code FAS-415, FA, 30g., gravimetric finish).
Soil samples are dried at low temperature,
screened to 80 mesh (MSA code PRP-757), a 15 grams portion is then
assayed for a multi-elements suite (MSA code IMS-136, Aqua Regia
digestion, ICP-AES/MS finish).
Quality assurance / Quality control
(QA/QC)
The MSA Analytical Laboratory is a qualified
assayer that performs and makes available internal assaying
controls. Duplicates, certified blanks and standards are
systematically used (1 control sample every 20-25 samples) as part
of CESA’s QA/QC program. Rejects, a 100 g pulp for each rock
sample, are stored for future use and controls.
Investor Inquiries
Further information is available on
Cornerstone’s website: www.cornerstoneresources.com and on
Twitter. For investor, corporate or media inquiries, please contact
ir@cornerstoneresources.ca, or:
Investor Relations: Mario Drolet; Email: Mario@mi3.ca; Tel.
(514) 904-1333
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at http://www.cornerstoneresources.com.
Cautionary Notice:This news
release may contain ‘Forward-Looking Statements’ that involve risks
and uncertainties, such as statements of Cornerstone’s beliefs,
plans, objectives, strategies, intentions and expectations. The
words “potential,” “anticipate,” “forecast,” “believe,” “estimate,”
“intend”, “trends”, “indicate”, “expect,” “may,” “should,” “could”,
“project,” “plan,” or the negative or other variations of these
words and similar expressions are intended to be among the
statements that identify ‘Forward-Looking Statements.’ Although
Cornerstone believes that its expectations reflected in these
‘Forward-Looking Statements’ are reasonable, such statements may
involve unknown risks, uncertainties and other factors disclosed in
our regulatory filings, viewed on the SEDAR website at
www.sedar.com. For us, uncertainties arise from the behaviour of
financial and metals markets, predicting natural geological
phenomena and from numerous other matters of national, regional,
and global scale, including those of an environmental, climatic,
natural, political, economic, business, competitive, or regulatory
nature. These uncertainties may cause our actual future results to
be materially different than those expressed in our Forward-Looking
Statements. Although Cornerstone believes the facts and information
contained in this news release to be as correct and current as
possible, Cornerstone does not warrant or make any representation
as to the accuracy, validity or completeness of any facts or
information contained herein and these statements should not be
relied upon as representing its views after the date of this news
release. While Cornerstone anticipates that subsequent events may
cause its views to change, it expressly disclaims any obligation to
update the Forward-Looking Statements contained herein except where
outcomes have varied materially from the original statements.
On behalf of the Board, Brooke MacdonaldPresident and CEO
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.
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