Sabina Gold & Silver Corp (SBB.T/SGSVF.OTCQX), (“Sabina” or the
“Company”) is pleased to provide final results from the 2020
exploration program at the Company’s 100% owned Back River Gold
Project, (“Back River” or the “Project”) Nunavut, Canada.
During the season, the Company completed
approximately 8,000 meters of drilling at Goose in addition to
completion of an extensive airborne geophysical Versatile Time
Domain Electromagnetic “VTEM” survey over the Goose, George and Del
properties.
Previously reported drilling this year includes
significant intercepts within the high-grade underground corridor
at the Umwelt V2 zone. (See news releases dated August 20,
September 3 and October 13, 2020).
The emergence and confirmation through drilling
of the V2 zone will result in an updated reserve estimate and has
provided the basis upon which to re-envision our development plans,
focusing on early mining of this high-grade underground material
into the mine life first. This drilling further highlights the
exceptional nature of the Goose site gold structures.
Drilling outside of the Umwelt high grade
corridor was completed at five target areas that include the Llama
Extension zone (3 drill holes), the Umwelt underground hinge zone
(3 drill holes) and the Hook, Jackaroo and Hackles targets (3 drill
holes). See attached map for target locations.
Highlights from these results include hole
20GSE585 returning 3.74 g/t Au over 43.70 m including 22.40 g/t Au
over 2.00 m intersecting the anticline hinge of the Umwelt
underground, see table 1 for details. This hole is a further
example of the wide zones encountered at the Goose deposits and was
drilled to expand the mineralization encountered in the Umwelt
underground to adjacent favourable structural traps.
Hole 20GSE577 from the Llama Extension zone,
where additional drilling was required to inform an initial
inferred resource estimate on this new zone, returned 3.75 g/t Au
over 9.15 m, including 8.04 g/t au over 3.40m.
Hole 20GSE580 returning 1.90 g/t Au over 13.7 m,
including 5.71 g/t Au over 1.00 m at the Hook prospect, targeted a
potential bridging zone between the Goose Main and Nuvuyak
deposits. While the hole overcut its target, it provided further
information for future drill testing.
Significant assay interval results are detailed
in table 1 and represent several strong advancements for geologic
modeling, gold zone vectoring and refinement of new exploration
targets. Results from a number of these target areas support
additional follow-up. A complete listing of all previously pending
assay results for the 2020 drilling program are detailed in table
2.
“Sabina is proud to have delivered a number of
significant exploration successes this year,” said Bruce McLeod,
President & CEO “This was accomplished while operating within a
restricted safety framework that has protected our employees,
contractors and community partners from COVID. At Umwelt, drilling
confirmed our team’s hypothesis of a high-grade underground
corridor with the definition of the V2 zone, which can provide
positive impacts to our project economics. Additional
resource style drill holes at the Llama Extension target as well as
internal work has enabled resource modelling for new inferred
resources at both Llama Extension and Nuvuyak zones. These two
oncoming resources have the potential to form the foundation for
future design of two new underground mines at the Goose site. With
this year’s challenges, our exploration targeting programs were
restricted but we have created good momentum for successful follow
up with the results from these drill holes. In addition, the
completion of a VTEM survey over some of the historically
underexplored and high value portions of our Back River properties
continues to demonstrate the prospectivity of this emerging mining
belt. We look forward to planning our exploration priorities in
2021 as we continue to evolve the world class nature of the Back
River Gold district.”
Table 1.0 – Selected Significant Intercepts from
2020 Exploration Drilling
Hole ID |
Area |
Azimuth& Dip |
EastingUTM |
NorthingUTM |
HoleDepth(m) |
From(m) |
To(m) |
Length(m) |
Au(g/t) |
Lithology |
20GSE577 |
LL |
226/-65 |
429625 |
7271693 |
671 |
586.7 |
595.85 |
9.15 |
3.75 |
Iron Formation |
incl. |
|
|
|
|
|
588 |
591.4 |
3.40 |
8.04 |
Iron Formation |
incl. |
|
|
|
|
|
588 |
588.5 |
0.50 |
18.40 |
Iron Formation |
20GSE578 |
LL |
59/-71 |
429255 |
7271340 |
586 |
565 |
574 |
9.00 |
2.21 |
Iron Formation |
incl. |
|
|
|
|
|
565 |
566 |
1.00 |
13.25 |
Iron Formation |
20GSE579B |
LL |
228/-66 |
429764 |
7271426 |
695 |
671.3 |
675 |
3.70 |
4.21 |
Iron Formation |
incl. |
|
|
|
|
|
673.25 |
674.1 |
0.85 |
13.20 |
Iron Formation |
20GSE580 |
HK |
33/-63 |
433119 |
7269189 |
785 |
626.7 |
640.4 |
13.70 |
1.90 |
Iron Formation |
incl. |
|
|
|
|
|
633 |
634 |
1.00 |
5.71 |
Iron Formation |
20GSE585 |
UM |
229/-50 |
429960 |
7270855 |
251 |
175.05 |
218.75 |
43.70 |
3.74 |
Iron Formation & Felsic Dyke |
incl. |
|
|
|
|
|
176.35 |
178.35 |
2.00 |
22.40 |
Iron Formation & Felsic Dyke |
and |
|
|
|
|
|
182.00 |
183.00 |
1.00 |
15.15 |
Quartz Vein |
and |
|
|
|
|
|
191.55 |
192.25 |
0.70 |
59.00 |
Quartz Vein |
and |
|
|
|
|
|
195.30 |
195.85 |
0.55 |
45.00 |
Quartz Vein |
20GSE586 |
UM |
230/-59 |
430194 |
7270697 |
347 |
316.10 |
320.00 |
3.90 |
3.77 |
Iron Formation |
incl. |
|
|
|
|
|
318.60 |
319.20 |
0.60 |
11.75 |
Iron Formation |
20GSE587 |
UM |
45/-60 |
429825 |
7270665 |
224 |
191.20 |
194.15 |
2.95 |
1.91 |
Iron Formation |
20GSE588 |
Hack |
229/-59 |
432968 |
7270502 |
320 |
285.30 |
286.45 |
1.15 |
1.40 |
Iron Formation |
^ True widths of the intercepts reported are unknown at this
time.
A photo accompanying this announcement is available at
https://www.globenewswire.com/NewsRoom/AttachmentNg/298e0563-2f7b-4dfc-aeb9-0a8e880df6ec
Exploration Drilling Results
At Llama Extension three widely spaced drill
holes tested discrete portions of the 500 m mineralization trend
with a main purpose of increasing resolution of the gold
mineralization shape boundaries and the geologic modelling of key
areas in support of an initial resource calculation. Drilling also
aimed to follow up coarse grained arsenopyrite-bearing structures
identified within the main D1 axial plane from previous drilling.
New drilling results provided additional data for input to the
resource model that are highlighted by assay intercepts returning
of 3.75 g/t Au over 9.15 m including 8.03 g/t Au over 3.00 m in
drill hole 20GSE577 targeting the area of the arsenopyrite
structures.
At the Umwelt anticline hinge target, outside of
the main mineralizing corridor of the V2 zone, three drill holes
tested a ~300 m plunge extent of lesser resolved, favourably folded
iron formation stratigraphy. The three holes successfully
intersected mineralization over significant widths, such as 3.74
g/t Au over 43.70 m in drill hole 20GSE585, that continues to
support additional follow up opportunities in resource growth.
The Hook target is a potential bridging zone
between the Goose Main and Nuvuyak deposits, with a strike length
of 600 m which hosts a large volume of iron formation with
indications of strong zones of mineralization. One drill hole test
targeted a complex D2 cross fold setting that extends south from
the Nuvuyak zone. Drill hole 20GSE580, returning 1.90 g/t Au over
13.7 m, is the first focused test in establishing the continuity of
the mineralization controls between the Nuvuyak and Goose Main
deposits. The drill hole aimed to test the lower portion of the
folded iron formation structure however ultimately over cut a
portion of the main target stratigraphy setting up improved
guidance for additional testing that may be achieved for 2021.
Geophysics Program
As previously reported, exploration activities
included an airborne VTEM geophysical survey over the Goose, George
and Del properties. The VTEM system was selected for the deep
penetrating transmitting and receiving capabilities allowing for
deeper structures and electromagnetic responses to be detected.
First phase 3D modelling of the 2020 VTEM data has been successful
in calibrating results and characterizing key elements over known
deposits, showing strong conductors centered on the Llama, Umwelt
and Goose Main deposits. Typically, two types of VTEM responses are
observed; broad single peak anomalies where conductors are
typically modelled at higher than 100 Siemen (i.e Umwelt), and
broad double peak anomalies from thin sheet-like conductors with
extensive strike length and depth extent with a lower conductance
of 10 Siemen (i.e. Locale 2 at the George Property).
This modelling has led to the geophysical
characterization of key known deposits enabling the evaluation
through comparison and prioritization of new and previously
identified geophysical anomalies. The second phase of result
modelling using deposit response characteristics is well advanced,
with initial targeting showing anomalous responses at the Goose
property down plunge of the Umwelt deposit, and in the Jackaroo and
Hackles areas. The completion of this second phase will facilitate
exploration targeting in 2021 at the Goose, George and Del
properties.
Table 2.0 – Significant Results from 2020
Exploration Drilling and Previously Pending Assays
Hole ID |
Area |
Azimuth& Dip |
EastingUTM |
NorthingUTM |
HoleDepth(m) |
From(m) |
To(m) |
Length(m) |
Au(g/t) |
Lithology |
20GSE575C* |
UM |
226/-47 |
430131 |
7270882 |
368 |
327.25 |
328.25 |
1.00 |
4.67 |
Greywacke |
20GSE577 |
LL |
226/-65 |
429625 |
7271693 |
671 |
522.80 |
523.3 |
0.50 |
1.72 |
Quartz Vein |
|
|
|
|
|
|
586.70 |
595.85 |
9.15 |
3.75 |
Iron Formation |
incl. |
|
|
|
|
|
588.00 |
591.40 |
3.40 |
8.04 |
Iron Formation |
incl. |
|
|
|
|
|
588.00 |
588.50 |
0.50 |
18.40 |
Iron Formation |
|
|
|
|
|
|
625.05 |
625.80 |
0.75 |
5.59 |
Iron Formation |
|
|
|
|
|
|
627.30 |
629.85 |
2.55 |
7.36 |
Iron Formation |
incl. |
|
|
|
|
|
628.35 |
629.00 |
0.65 |
18.00 |
Iron Formation |
|
|
|
|
|
|
632.40 |
632.90 |
0.50 |
2.12 |
Iron Formation |
|
|
|
|
|
|
634.10 |
634.60 |
0.50 |
3.60 |
Iron Formation |
20GSE578 |
LL |
59/-71 |
429255 |
7271340 |
586 |
490.20 |
491.15 |
0.95 |
2.03 |
Iron Formation |
|
|
|
|
|
|
554.30 |
555.30 |
1.00 |
1.61 |
Iron Formation |
|
|
|
|
|
|
565.00 |
574.00 |
9.00 |
2.21 |
Iron Formation |
incl. |
|
|
|
|
|
565.00 |
566.00 |
1.00 |
13.25 |
Iron Formation |
20GSE579 |
LL |
228/-65 |
429765 |
7271427 |
101 |
DDH Abandoned - No Significant Values |
20GSE579B |
LL |
228/-66 |
429764 |
7271426 |
695 |
607.00 |
608.00 |
1.00 |
4.44 |
Iron Formation |
|
|
|
|
|
|
619.20 |
620.20 |
1.00 |
13.10 |
Greywacke |
|
|
|
|
|
|
660.90 |
666.15 |
5.25 |
1.13 |
Iron Formation |
|
|
|
|
|
|
671.30 |
675.00 |
3.70 |
4.21 |
Iron Formation |
incl. |
|
|
|
|
|
673.25 |
674.10 |
0.85 |
13.20 |
Iron Formation |
20GSE580 |
HK |
33/-63 |
433119 |
7269189 |
785 |
123.00 |
124.00 |
1.00 |
1.02 |
Iron Formation |
|
|
|
|
|
|
506.70 |
509.55 |
2.85 |
2.35 |
Iron Formation |
|
|
|
|
|
|
538.30 |
539.00 |
0.70 |
2.98 |
Iron Formation |
|
|
|
|
|
|
599.00 |
600.55 |
1.55 |
3.00 |
Iron Formation |
|
|
|
|
|
|
626.70 |
640.40 |
13.70 |
1.90 |
Iron Formation |
incl. |
|
|
|
|
|
633.00 |
634.00 |
1.00 |
5.71 |
Iron Formation |
|
|
|
|
|
|
773.90 |
774.90 |
1.00 |
4.45 |
Iron Formation |
20GSE582* |
UM |
229/-56 |
430182 |
7270849 |
356 |
274.60 |
275.70 |
1.10 |
2.01 |
Iron Formation |
|
|
|
|
|
|
278.45 |
279.30 |
0.85 |
13.70 |
Greywacke |
|
|
|
|
|
|
339.40 |
341.50 |
2.10 |
5.91 |
Greywacke |
|
|
|
|
|
|
347.10 |
347.80 |
0.70 |
1.78 |
Greywacke |
20GSE583 |
JK |
220/-50 |
430819 |
7269610 |
464 |
No Significant Values |
20GSE585 |
UM |
229/-50 |
429960 |
7270855 |
251 |
152.35 |
153.90 |
1.55 |
1.87 |
Iron Formation |
|
|
|
|
|
|
158.40 |
159.45 |
1.05 |
1.23 |
Iron Formation |
|
|
|
|
|
|
165.00 |
170.85 |
5.85 |
1.67 |
Iron Formation |
|
|
|
|
|
|
175.05 |
218.75 |
43.70 |
3.74 |
Iron Formation & Felsic Dyke |
incl. |
|
|
|
|
|
176.35 |
178.35 |
2.00 |
22.40 |
Iron Formation & Felsic Dyke |
and |
|
|
|
|
|
182.00 |
183.00 |
1.00 |
15.15 |
Quartz Vein |
and |
|
|
|
|
|
191.55 |
192.25 |
0.70 |
59.00 |
Quartz Vein |
and |
|
|
|
|
|
195.30 |
195.85 |
0.55 |
45.00 |
Quartz Vein |
20GSE586 |
UM |
230/-59 |
430194 |
7270697 |
347 |
289.20 |
290.35 |
1.15 |
1.40 |
Iron Formation |
|
|
|
|
|
|
301.15 |
301.85 |
0.70 |
5.90 |
Iron Formation |
|
|
|
|
|
|
316.10 |
320.00 |
3.90 |
3.77 |
Iron Formation |
incl. |
|
|
|
|
|
318.60 |
319.20 |
0.60 |
11.75 |
Iron Formation |
|
|
|
|
|
|
323.55 |
326.00 |
2.45 |
2.05 |
Iron Formation |
|
|
|
|
|
|
331.90 |
335.00 |
3.10 |
2.97 |
Iron Formation |
20GSE587 |
UM |
45/-60 |
429825 |
7270665 |
224 |
191.20 |
194.15 |
2.95 |
1.91 |
Iron Formation |
|
|
|
|
|
|
197.45 |
200.40 |
2.95 |
1.68 |
Iron Formation |
|
|
|
|
|
|
203.50 |
204.35 |
0.85 |
1.55 |
Iron Formation |
20GSE588 |
Hack |
229/-59 |
432968 |
7270502 |
320 |
285.30 |
286.45 |
1.15 |
1.40 |
Iron Formation |
*Additional intervals from previously released drill holes. |
^ True widths of the intercepts reported are unknown at this
time. |
Qualified Persons
The Qualified Person as defined by NI 43-101 as
pertains to the Back River Project, is James Maxwell, Director of
Exploration, for the Company. All drill core samples selected
within the exploration program are subject to a company standard of
internal quality control and quality assurance programs which
include the insertion of certified reference materials, blank
materials and duplicates analysis. All samples are sent to ALS
Global laboratories located in Vancouver, British Columbia where
they are processed for gold analysis by 50 gram fire assay with
finish by a combination of atomic absorption and gravimetric
methods. Additionally, analysis by screen metallic processes is
performed on select samples. ALS Global quality systems conform to
requirements of ISO/IEC Standard 17025 guidelines and meets assay
requirements outlined for NI 43-101.
Sabina Gold & Silver Corp.
Sabina Gold & Silver Corp. is well-financed
and is an emerging precious metals company with district scale,
advanced, high grade gold assets in one of the world’s newest,
politically stable mining jurisdictions: Nunavut, Canada.
Sabina released a Feasibility Study on its 100%
owned Back River Gold Project which presents a project that has
been designed on a fit-for purpose basis, with the potential to
produce ~200,000 ounces a year for ~11 years with a rapid payback
of 2.9 years (see “Technical Report for the Initial Project
Feasibility Study on the Back River Gold Property, Nunavut, Canada”
dated October 28, 2015).
The Project received its final Project
Certificate on December 19, 2017. The Project received its Type A
Water License on November 14, 2018 and its listing to enable
deposition of tailings on Schedule 2 of the Metals and Diamond
Mining Effluent Regulations on June 25, 2020. The Company is now in
receipt of all major authorizations for construction and
operations.
In addition to Back River, Sabina also owns a
significant silver royalty on Glencore’s Hackett River Project. The
silver royalty on Hackett River’s silver production is comprised of
22.5% of the first 190 million ounces produced and 12.5% of all
silver produced thereafter.
For further information please contact:
Nicole Hoeller, Vice-President,
Communications: 1 888 648-4218
nhoeller@sabinagoldsilver.com
Forward Looking InformationThis
news release contains “forward-looking information” within the
meaning of applicable securities laws (the “forward-looking
statements”), including our belief as to the extent, results and
timing of and various studies relating to engineering studies,
infrastructure improvement activities, exploration results and
permitting and licensing outcomes. These forward-looking statements
are made as of the date of this news release. Readers are cautioned
not to place undue reliance on forward-looking statements, as there
can be no assurance that the future circumstances, outcomes or
results anticipated in or implied by such forward-looking
statements will occur or that plans, intentions or expectations
upon which the forward-looking statements are based will occur.
While we have based these forward-looking statements on our
expectations about future events as at the date that such
statements were prepared, the statements are not a guarantee that
such future events will occur and are subject to risks,
uncertainties, assumptions and other factors which could cause
events or outcomes to differ materially from those expressed or
implied by such forward-looking statements. Such factors and
assumptions include, among others, the effects of general economic
conditions, commodity prices, changing foreign exchange rates and
actions by government and regulatory authorities and misjudgments
in the course of preparing forward-looking statements. In addition,
there are known and unknown risk factors which could cause our
actual results, performance or achievements to differ materially
from any future results, performance or achievements expressed or
implied by the forward-looking statements. Known risk factors
include risks associated with exploration and project development;
the need for additional financing; the calculation of mineral
resources and reserves; operational risks associated with mining
and mineral processing; fluctuations in metal prices; title
matters; government regulation; obtaining and renewing necessary
licenses and permits; environmental liability and insurance;
reliance on key personnel; the potential for conflicts of interest
among certain of our officers or directors; the absence of
dividends; currency fluctuations; labour disputes; competition;
dilution; the volatility of the our common share price and volume;
future sales of shares by existing shareholders; and other risks
and uncertainties, including those relating to the Back River
Project and general risks associated with the mineral exploration
and development industry described in our Annual Information Form,
financial statements and MD&A for the fiscal period ended
December 31, 2019 filed with the Canadian Securities Administrators
and available at www.sedar.com. Although we have attempted to
identify important factors that could cause actual actions, events
or results to differ materially from those described in
forward-looking statements, 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 forward-looking statements
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 statements. We are under no obligation to update or
alter any forward-looking statements except as required under
applicable securities laws. This news release has been authorized
by the undersigned on behalf of Sabina Gold & Silver Corp.
Bruce McLeod, President & CEOSuite 1800 – Two
Bentall Centre555 Burrard StreetVancouver, BC V7X 1M7Tel 604
998-4175 Fax 604
998-1051http://www.sabinagoldsilver.com
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