Adventus Zinc Corporation (“Adventus”)
(TSX-V:ADZN) and
Salazar Resources Limited
(“Salazar”) (TSX-V:SRL) are pleased to announce the
commencement of an extensive surface exploration program for 2018
at the 21,537-hectare Curipamba project located in Ecuador
(“Curipamba Project”). The 2018 regional work program at the
Curipamba Project is based upon a thorough target generation review
of a large historical database that includes prospecting,
geological mapping, surficial geochemistry, geophysics and
drilling. Adventus and Salazar are confident their methodical
approach will result in positive outcomes, and greatly improve
their knowledge and understanding of mineralizing system
surrounding the El Domo volcanogenic massive sulphide deposit (“El
Domo”). Work in 2018 is primarily targeting new VMS
discoveries, and kick-off programs have commenced at the Sesmo
target.
The Curipamba Project hosts El Domo and more
than a dozen underexplored precious metal enriched targets;
however, when Salazar discovered El Domo in Q1 2008 (see February
28, 2008 Salazar news release), focus shifted away from the
regional targets and towards Mineral Resource definition
drilling. Salazar’s subsequent work programs have resulted in
the current Mineral Resource estimate for El Domo that consists of
6.08 Mt grading 2.33% Cu, 3.06% Zn, 0.28% Pb, 2.99 g/t Au and 55.8
g/t Ag in the Indicated category, and 3.88 Mt grading 1.56% Cu,
2.19% Zn, 0.16% Pb, 2.03 g/t Au and 42.9 g/t Ag in the Inferred
category (see January 16, 2015 Salazar news release). This
Mineral Resource estimate was part of a technical report filed on
SEDAR: “Curipamba Project - El Domo Deposit Amended and Restated
Preliminary Economic Assessment Central Ecuador” that was prepared
by Independent Qualified Persons Gustavo Calvo Martin, M.Sc.A., P.
Geo and Adam Johnston, B. Eng., FAusIMM.
Following completion of an agreement between
Adventus and Salazar in 2017 (see September 14, 2017 Adventus news
release); which included a significant Adventus work commitment,
the companies will not only advance the evaluation of the
development potential for El Domo, but more importantly, renew
regional exploration, starting with the targets previously
identified by Salazar.
Sesmo Target
At Sesmo, work started with a review of any
historical drill holes near the target; which is located 1,100
metres north of El Domo. This review will be followed by
prospecting, soil sampling, and a 22-line kilometres IP geophysical
survey, noting that the geophysical survey is key to refining
targets for drilling. No follow-up drilling to the channel
samples has been done. Adventus and Salazar anticipate
commencement of drilling in February 2018.
The Sesmo target is characterized by outcropping
high-grade gold and silver mineralization, in what Salazar
describes as a hydrothermal breccia. These hydrothermal
breccia units at Sesmo are hosted in a quartz-eye phyric dacite
volcanic rock, and possess mineralized, silicified, polymetallic
clasts in an argillic altered matrix. Previous surface
sampling by Salazar (see April 27, 2007 news release) reported a
15-metre channel sample grading 39.1 g/t Au and 741 g/t Ag that
included 186.5 g/t Au and 1,055 g/t Ag over 2 metres. No base
or other trace metal values were published by Salazar. Other
channel samples reported by Salazar from Sesmo include:
- 10 metres at 9.54 g/t gold and 634.0 g/t silver
- 3 metres at 12.30 g/t gold and 469.0 g/t silver
- 3 metres at 3.67 g/t gold and 12.0 g/t silver
Exploring Curipamba after
Sesmo
As noted previously, Sesmo target is one of over
a dozen important, previously known, precious metal-rich targets at
Curipamba Project. This includes, but is not limited to Cade,
Cade 1, Cade Sur, Roble, Roble 1, Roble Este, El Gallo, Sesmo Sur,
Agua Santa, and La Vaquera as shown in the “Curipamba Project Map
of Concessions” on www.adventuszinc.com.
Cade/Cade 1/Cade Sur
Targets
The Cade, Cade 1, and Cade Sur targets stretch
along a northeast-southwest trend, and are located 100 to 600
metres west of El Domo respectively. At the Cade 1 target,
Salazar noted in their May 17, 2007 news release that rock chip
sampling yielded 7 metres grading 9.80 g/t gold, 409.0 g/t silver,
and over 1% zinc. Mineralization is described as being hosted
in a hydrothermal breccia.
At Cade Sur, Salazar noted in a June 5, 2007
news release they described that mineralization is hosted in a
volcanic breccia, possessing polymetallic clasts in an argillic
altered matrix with disseminated pyrite. The most significant
channel sample from Cade Sur was 7.63 g/t gold and 291.0 g/t silver
over 10 metres; however, sampling also yielded a channel sample
grading 5.03 g/t gold, 376.0 g/t silver, 2.74% copper, and 19.6%
zinc over 1.30 metres.
Roble/Roble 1/Roble Este
Targets
The Roble and Roble 1 targets stretch along an
east-west trend, and are located 100 metres north of El Domo.
Salazar, in their October 18, 2007 news release, noted that channel
sampling of outcrops along a mineralized trend at Roble 1 yielded a
3.60 metre sample grading 15.12 g/t gold and 258.0 g/t silver;
which also had 0.56% copper, 3.25% lead, and 5.25% zinc. This
included a 0.93 metre subsection grading 35.29 g/t gold, 630.0 g/t
silver, 1.36% copper, 7.98% lead, and 12.80% zinc.
Mineralization at surface and appears open;
however, it appears the massive sulphide mineralization has been
structurally complicated by a fault structure. Semi-massive to
massive sulphide clasts are present along the fault structure and
range in size from 0.05 to 1.00 metres in diameter.
In Salazar’s April 18, 2008 MDA filed on SEDAR,
they noted Roble 1 was tested by five drill holes totaling 1,015
metres which confirmed the presence of fault-related semi-massive
to massive sulphide mineralization, and the presence of
hydrothermal breccia units with stockwork-like base metal
mineralization. Highlights of this work are summarized in
Table 1 in the news release Appendix.
At Roble, two other channel samples yielded 1.00
g/t gold, 95.0 g/t silver, 4.40% copper, and 3.00% zinc over 4.0
metres; including 2.4 g/t gold, 295.0 g/t silver, 15.1% copper, and
6.9% zinc over 1.0 metres; and 1.1 g/t gold, 3.2 g/t silver, and
3.2% copper over 2.2 metres. In Salazar’s April 18, 2008 MDA
filed on SEDAR, they noted Roble and Roble Este was tested by three
drill holes totalling 731 metres that did confirm the presence of
fault-related semi-massive to massive sulphide mineralization, and
the presence of hydrothermal breccia units with stockwork-like base
metal mineralization. Highlights of this work are summarized
in Table 2 in the Appendix at end of the news release.
El Gallo Target
The El Gallo target is located approximately 420
metres directly south of El Domo. It is an important target
because the favourable strata between El Domo and the El Gallo
target remains relatively untested. The mineralization at El
Gallo is hosted in a volcanic breccia unit containing
polymetallic-barite clasts that occur in argillic altered
matrix. This is interpreted to be a resedimented slump
breccia downslope from the volcanic edifice that is the foci for
formation of the upper baritic and precious metal-rich portion of
massive sulphide mineralization at El Domo or another nearby
unknown VMS deposit.
In Salazar’s March 20, 2007 news release, they
noted that channel sampling of outcrops along a mineralized trend
in a creek bed that yielded a 17-metre sample grading 11.2 g/t gold
and 505.0 g/t silver. Other channel samples reported by
Salazar from El Gallo include:
- 12 metres at 7.09 g/t gold and 299 g/t silver
- 10 metres at 12.13 g/t gold and 235.0 g/t silver
- 6 metres at 4.00 g/t gold and 38.0 g/t silver
A follow-up drill program at El Gallo noted
assay results from four drill holes (see January 21, 2008 Salazar
news release) and a fifth drill hole was disclosed by Salazar in
their March 12, 2008 news release. Highlights of this work
are summarized in Table 3 in the Appendix at end of the news
release.
Sesmo Sur Target
The Sesmo Sur target is located about 5.8
kilometres southwest of El Domo. It was initially called the
El Lobo target (see June 5, 2007 Salazar news release); however,
subsequent work identified a broader mineralized system, and the
area was renamed (see September 12, 2007 news release).
Mineralization at Sesmo Sur was characterized by
both barite and sulphide minerals hosted within an andesitic
volcanic breccia over an area of 350 metres by 50 metres that has
argillic and silica-pyrite alteration both to the east and west of
the target. However, the initial discovery was highlighted by
a 68-metre channel sample grading 2.6 g/t gold and 82 g/t silver;
which included 5 metres grading 8.5 g/t gold and 304 g/t silver
(see June 5, 2007 news release). Other channel samples reported by
Salazar from Sesmo Sur include:
- 44 metres at an average of 3.21 g/t gold and 15.0 g/t
silver
- 52 metres at an average of 3.71 g/t gold and 162.0 g/t
silver
- 29 metres at an average of 2.66 g/t gold and 14.0 g/t
silver
- 12 metres at an average of 1.07 g/t gold and 183.0 g/t
silver
Salazar followed up the successful surface
exploration at Sesmo Sur with drilling a total of 3,746 metres in
eighteen drill holes (see February 28, 2008 Salazar news
release). Highlights of this work are summarized in Table 4
in the Appendix at end of the news release.
Although extensive gold and silver
mineralization was identified on surface, and the hydrothermal
breccia units were successfully intersected by drilling, more work
is required to understand the nature and distribution of both
precious and base metals in this mineralizing system at Sesmo
Sur.
La Vaquera Target
During regional exploration work in 2007 about 2
kilometres west of the Sesmo Sur target, fourteen float boulder and
outcrop grab samples were collected in the La Vaquera area that
contained gold and silver mineralization. Values ranged
between 0.01 to 16.30 g/t gold and 0.1 to 136.1 g/t silver.
Geochemical results also showed a wide range of copper, lead and
zinc.; however, it was copper that provided the best corresponding
results. In addition, Salazar staff collected 256 soil samples that
produced a geochemical anomaly for gold greater than 100 ppb of
approximately 200 metres in length. Full maps for La Vaquera
target, and its tabulated geochemical results can be seen in the
February 28, 2008 Salazar news release.
Agua Santa Target
Prospecting activities about 1.5 kilometres
north of the Sesmo Sur target yielded numerous large float boulder
samples characterized by jasper and what was described as
hydrothermal breccia that possessed barite, pyrite, and
sphalerite. Further investigation revealed a broad
geochemical anomaly. Values for gold and silver ranged
between 0.01 to 4.99 g/t gold, and 0.1 to 496.0 g/t silver; whereas
base metal values graded up to 0.42% copper, 0.99% lead, and 2.89%
zinc. Full maps for the Agua Santa target and its tabulated
geochemical results can be seen in the February 28, 2008 Salazar
news release.
El Domo Mineral Resource
Update
Adventus has retained Roscoe Postle Associates
Inc. to complete an updated Mineral Resource estimate for El Domo.
The updated Mineral Resource estimate will be prepared in
accordance with Canadian Institute of Mining, Metallurgy, and
Petroleum (“CIM”) Standards on Mineral Resources and Reserves –
Definitions and Guidelines, as referred to in National Instrument
(“NI”) 43-101, and adopted by CIM Council on May 10, 2014.
This updated Mineral Resource estimate will include all relevant
information from Salazar’s 2017 Phase V drilling program that
included 33 drill holes totaling 9,765 metres on El Domo (see
September 8, 2017 Salazar news release). Adventus anticipates
that the Mineral Resource update will be available in Q1 2018.
The technical information of this news release
has been reviewed and verified as accurate by Mr. Jason Dunning,
M.Sc., P.Geo., Vice President Exploration for Adventus, a
non-Independent Qualified Person, as defined by NI 43-101.
About Adventus
Adventus is a well-financed and unique company
focused on zinc exploration and project development globally. Its
strategic shareholders include Altius Minerals Corporation,
Greenstone Resources LP, and Resource Capital Funds; as well as
other highly respected investors in the mining business.
Adventus currently has large prospective land packages in both
Ireland and Newfoundland and Labrador, Canada, and is earning a 75%
ownership interest in the Curipamba copper-gold-zinc project in
Ecuador. In addition, Adventus has a country-wide generative
exploration alliance with its partners in Ecuador. Adventus is
based in Toronto, Canada, and is listed on the TSX-V under the
symbol ADZN.
About Salazar
Salazar is a publicly-listed mineral resource
company engaged in the exploration and development of new highly
prospective areas in Ecuador. Led by a senior Ecuadorian
management team and most notably by its namesake Fredy Salazar,
this team has been instrumental in other major discoveries
throughout Ecuador, including Aurelian's Fruta Del Norte discovery,
Mozo Deposit, Ex Newmont's Cangrejos Project and International
Minerals Rio Blanco and Gaby Deposit. Being an
Ecuadorian-based company gives the Company a strategic advantage
enabling the Company to complete exploration at a rapid pace.
With an excellent property portfolio (6 projects – 33,383
hectares), good geopolitical positioning and a number of strategic
corporate and financial partnerships, Salazar has positioned itself
to be a strategic player in
Ecuador.
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 news release.
This press release contains “forward -looking
information” within the meaning of applicable Canadian securities
laws. Any statements that express or involve discussions with
respect to predictions, expectations, beliefs, plans, projections,
objectives, assumptions or future events or performance (often, but
not always, identified by words or phrases such as “believes”,
“anticipates”, “expects”, “is expected”, “scheduled”, “estimates”,
“pending”, “intends”, “plans”, “forecasts”, “targets”, or “hopes”,
or variations of such words and phrases or statements that certain
actions, events or results “may”, “could”, “would”, “will”,
“should” “might”, “will be taken”, or “occur” and similar
expressions) are not statements of historical fact and may be
forward-looking statements.
Forward-looking information herein includes, but
is not limited to, statements that address activities, events or
developments that Adventus and Salazar expect or anticipate will or
may occur in the future. Although Adventus and Salazar has
attempted to identify important factors that could cause actual
actions, events or results to differ materially from those
described in forward-looking information, there may be other
factors that cause actions, events or results not to be as
anticipated, estimated or intended. There can be no assurance that
such information will prove to be accurate, and actual results and
future events could differ materially from those anticipated in
such information. Accordingly, readers should not place undue
reliance on forward-looking information. Adventus and Salazar
undertakes to update any forward-looking information except in
accordance with applicable securities laws.
For further information from Adventus, please
contact Christian Kargl-Simard, Chief Executive Officer, at
1-416-230-3440 or christian@adventuszinc.com.
For further information from Salazar, please
contact ir@salazarresources.com.
APPENDIX:
Table 1: Summary of historical drilling results from
Roble 1
Drill Hole |
From(m) |
To(m) |
Thickness(m) |
Au (g/t) |
Ag (g/t) |
Cu (%) |
Pb (%) |
Zn (%) |
True Thickness (m) |
CURI-07-021 |
121.52 |
139.00 |
17.48 |
0.04 |
4.96 |
0.04 |
0.00 |
0.65 |
(3) |
CURI-07-025 |
101.80 |
162.95 |
61.15 |
0.18 |
4.07 |
0.05 |
0.04 |
0.70 |
(3) |
CURI-08-029 |
11.00 |
19.00 |
8.00 |
1.71 |
31.0 |
0.00 |
0.01 |
0.05 |
(3) |
|
87.00 |
107.00 |
20.00 |
1.00 |
29.04 |
0.03 |
0.19 |
0.41 |
(3) |
CURI-07-020 |
11.59 |
13.84 |
2.25 |
0.13 |
58.17 |
0.04 |
0.18 |
0.47 |
(3) |
Notes:
- Drill holes CURI-07-019 did not have any significant
results
- QAQC for drill results is summarized in the April 18, 2008 MDA
filed on SEDAR by Salazar.
- Salazar did not publish any true thickness estimates for Roble
1 in the April 18, 2008 MDA filed on SEDAR due to a lack of
geological information on the orientation of host strata.
Additional geological mapping and drilling is required to
facilitate true thickness determinations
Table 2: Summary of historical drilling
results from Roble
Drill Hole |
From(m) |
To(m) |
Thickness(m) |
Au (g/t) |
Ag (g/t) |
Cu (%) |
Pb (%) |
Zn (%) |
True Thickness (m) |
CURI-07-022 |
19.73 |
25.18 |
5.45 |
2.82 |
34.4 |
2.14 |
0.06 |
0.95 |
(3) |
including |
19.73 |
22.86 |
3.13 |
4.77 |
53.4 |
3.69 |
0.10 |
1.62 |
(3) |
|
195.63 |
224.00 |
28.37 |
0.17 |
8.81 |
0.03 |
0.05 |
0.28 |
(3) |
CURI-07-024 |
15.00 |
35.30 |
20.30 |
0.40 |
5.51 |
0.06 |
0.09 |
0.67 |
(3) |
Notes:
- Drill holes CURI-07-023 did not have any significant
results
- QAQC for drill results is summarized in the April 18, 2008 MDA
filed on SEDAR by Salazar.
- Salazar did not publish any true thickness estimates for Roble
in the April 18, 2008 MDA filed on SEDAR due to a lack of
geological information on the orientation of host strata.
Additional geological mapping and drilling is required to
facilitate true thickness determinations
Table 3: Summary of historical drilling
results from El Gallo
Drill Hole |
From(m) |
To(m) |
Thickness(m) |
Au (g/t) |
Ag (g/t) |
Cu (%) |
Pb (%) |
Zn (%) |
True Thickness (m) |
CURI-07-015 |
8.05 |
15.00 |
6.95 |
4.51 |
157.0 |
0.12 |
0.06 |
0.04 |
(3) |
CURI-07-016 |
0.00 |
8.25 |
8.25 |
5.80 |
66.0 |
0.08 |
0.09 |
0.04 |
(3) |
Including |
2.00 |
7.00 |
5.00 |
9.12 |
104.0 |
0.09 |
0.10 |
0.04 |
(3) |
CURI-07-017 |
6.09 |
10.66 |
4.57 |
9.45 |
337.8 |
0.20 |
0.23 |
0.25 |
(3) |
Including |
6.09 |
9.00 |
2.91 |
14.42 |
512.1 |
0.28 |
0.27 |
0.29 |
(3) |
CURI-07-018 |
13.30 |
18.28 |
4.98 |
3.33 |
17.8 |
0.05 |
0.37 |
0.03 |
(3) |
Notes:
- Drill holes CURI-07-014 did not have any significant
results
- QAQC for drill results is summarized in the January 21, 2008
and March 12, 2008 Salazar news releases.
- Salazar did not publish any true thickness estimates for El
Gallo in either the January 21, 2008 or March 12, 2008 news
releases to a lack of geological information on the orientation of
host strata. Additional geological mapping and drilling is
required to facilitate true thickness determinations
Table 4: Summary of historical drilling
results from Sesmo Sur
Drill Hole |
From(m) |
To(m) |
Thickness(m) |
Au (g/t) |
Ag (g/t) |
Cu (%) |
Pb (%) |
Zn (%) |
True Thickness (m) |
CURI-07-001 |
6.09 |
18.00 |
11.91 |
2.25 |
31.0 |
0.20 |
0.27 |
0.60 |
(5) |
including |
12.00 |
16.00 |
4.00 |
2.21 |
23.0 |
0.09 |
0.23 |
1.61 |
(5) |
|
56.10 |
60.00 |
3.90 |
1.79 |
8.4 |
0.08 |
0.06 |
2.76 |
(5) |
|
104.00 |
110.00 |
6.00 |
0.41 |
5.2 |
0.25 |
0.00 |
0.02 |
(5) |
CURI-07-002 |
1.80 |
5.68 |
3.88 |
2.03 |
23.1 |
0.09 |
0.21 |
0.66 |
(5) |
|
15.24 |
22.86 |
7.48 |
1.31 |
20.0 |
0.11 |
0.11 |
1.70 |
(5) |
CURI-07-003 |
0.70 |
8.00 |
7.30 |
2.56 |
14.0 |
0.05 |
0.36 |
0.02 |
(5) |
|
41.14 |
79.24 |
38.10 |
0.63 |
15.37 |
0.10 |
0.23 |
0.67 |
(5) |
CURI-07-005 |
0.20 |
15.24 |
15.04 |
2.54 |
50.1 |
0.23 |
0.19 |
0.25 |
(5) |
including |
0.20 |
2.68 |
2.48 |
11.14 |
107.3 |
0.07 |
0.57 |
0.04 |
(5) |
CURI-07-009 |
0.40 |
16.00 |
15.60 |
1.45 |
17.4 |
0.17 |
0.10 |
0.04 |
(5) |
CURI-07-012 |
16.76 |
44.19 |
27.43 |
0.18 |
1.6 |
0.10 |
0.00 |
0.36 |
(5) |
|
57.00 |
68.50 |
11.50 |
0.20 |
1.6 |
0.04 |
0.02 |
0.51 |
(5) |
CURI-07-026 |
32.10 |
37.30 |
5.20 |
0.14 |
5.2 |
0.13 |
0.02 |
1.26 |
(5) |
Notes:
- Information also sourced from April 18, 2008 MDA filed on SEDAR
where necessary
- Drill holes CURI-004, 006, 007, 008, 010, 011, and 013; and
CURI-08-027, 028, 031, and 033; did not return any significant
results
- QAQC for drill results is summarized in the February 28, 2008
news release and April 18, 2008 MDA filed on SEDAR by Salazar.
- As cited from the November 27, 2007 MDA filed on SEDAR; “Holes
CURI-07-004, CURI-07-006, CURI-07-007, CURI-07-008, CURI-07-009,
most of the cores were lost during the camp invasion (approx. 50%)
and the remaining cores are currently being organized to be sent to
the Laboratory.”
- Salazar did not publish any true thickness estimates for Sesmo
Sur in the February 28, 2008 news release to a lack of geological
information on the orientation of host strata. Additional
geological mapping and drilling is required to facilitate true
thickness determinations
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