North American Nickel Inc. (TSX VENTURE:NAN)
(OTCBB:WSCRF) (CUSIP:65704T 108) (the "Company" or “NAN”) is
pleased to provide an exploration update and summary of significant
results on its 100% owned Maniitsoq nickel-copper-cobalt-PGM
project in Southwest Greenland.
In 2017, the Company implemented an $11.1M
exploration program consisting of 8,767 metres of diamond drilling
in 23 holes, two regional and four detailed induced
polarisation (IP) surveys covering 13km2, surface and borehole
electromagnetic (EM) surveys, borehole gyro, optical televiewer and
physical properties surveys, a comprehensive review of geochemistry
and petrology of the noritic intrusions, a surface geology sampling
and mapping program, and 3D modeling of the mineral zones.
PROJECT HIGHLIGHTS
- In 2017, the Company continued its systematic evaluation of the
depth extent of known mineral zones to identify thicker and more
extensive sheets of breccia-style mineralization. This work
continues to advance the understanding of the host intrusions and
refine geophysical targeting tools. The result has been the
intersection of significant nickel-copper sulphide mineralization
at multiple locations.
- The Mikissoq zone was extended by 60 meters down plunge; the
P-013 SE mineral zone was extended for 140m down-plunge and the
P-058 zone at Fossilik was extended to a vertical depth of 650 m.
Extensive zones of melanorite were mapped in the footprint of the
mineral zones of the Imiak Hill Complex (IHC) as well as
Fossilik.
- Petrological and geochemical studies of the differentiated
mafic intrusions underscores the importance of melanorite as a host
to high grade semi-massive breccia style nickel-copper sulphides
enveloped in a halo of lower grade mineralization.
- Interpretation of IP and gravity data coupled with petrology
and geochemistry highlights the potential for the known mineral
zones to expand in width within the adjacent melanorite
intrusions.
Follow-up in 2018 will focus attention on the
larger differentiated intrusions where more continuous zones of
high Ni tenor breccia style sulphide mineralization can be
identified by EM methods. The program of work will be driven by
electromagnetic methods that are sensitive to the core zones of
high grade Ni sulphide.
NAN CEO, Keith Morrison commented: “The
extensive occurrence of sulphide mineralization with high nickel,
copper and cobalt concentrations in sulphide continues to provide
the focus for exploration in depositional environments where
geological processes have concentrated the mineralization. The
importance of the larger bodies of melanorite as hosts to more
continuous zones of breccia style sulphide mineralization within a
halo of disseminated sulphide is an important driver to the
discovery of mineralization. Exploration in 2018 will focus
attention on potentially more continuous breccia style
mineralization contained in melanorite bodies at Fossilik and the
IHC.”
DRILLING
Drilling expanded the Mikissoq zone by 60 metres
in a down plunge direction (News Release dated October 10, 2017),
extended the P-013 SE mineral zone by 140m down-plunge (News
Release dated November 14, 2017), extended the P-058 zone to a
vertical depth of 650m (News Release dated November 23, 2017), and
encountered new nickel intersections at the P-004 target at
Fossilik (News Release dated December 18, 2017). The potential for
the mineralized zone at P-058 to extend into a larger melanorite
body is supported by geological, gravity, and IP data. The Mikissoq
zone breccia sulphide mineralization is also open at depth, but the
EM signature points back to the heart of the known mineral zone,
and the IP response related to the known near-surface disseminated
sulphide.
Table 1 gives a summary of selected drilling
highlights for each of these mineralized areas and a location map
(Figure 1) may be viewed using the link provided at the end of the
release.
TABLE 1: Selected 2017 Assay
Results from Mikissoq, Spotty Hill, P-058, P-004 and P-013
SE
Hole Number |
|
From (m) |
To(m) |
Core Length (m) |
Ni % |
Cu % |
Co % |
S % |
Pt g/t |
Pd g/t |
Au g/t |
*Ni Eq % |
IHC: Mikissoq |
MQ-17-135 |
|
359.85 |
435.60 |
75.75 |
1.10 |
0.43 |
0.03 |
4.02 |
0.03 |
0.02 |
0.07 |
1.54 |
|
incl. |
359.85 |
370.10 |
10.25 |
2.29 |
1.33 |
0.05 |
8.83 |
0.03 |
0.03 |
0.21 |
3.43 |
|
and |
416.35 |
435.60 |
19.25 |
1.89 |
0.26 |
0.04 |
6.70 |
0.03 |
0.02 |
0.02 |
2.32 |
|
incl. |
417.00 |
423.00 |
6.00 |
2.94 |
0.29 |
0.07 |
10.72 |
0.02 |
0.02 |
0.01 |
3.55 |
|
and |
425.90 |
426.20 |
0.30 |
9.55 |
0.80 |
0.24 |
28.98 |
0.31 |
0.19 |
0.11 |
11.57 |
IHC: Spotty Hill |
MQ-17-143 |
|
381.00 |
388.80 |
7.80 |
1.35 |
0.26 |
0.04 |
5.42 |
0.25 |
0.28 |
1.32 |
2.30 |
|
incl. |
381.00 |
386.00 |
5.00 |
1.69 |
0.33 |
0.05 |
6.89 |
0.33 |
0.34 |
2.04 |
3.02 |
|
incl. |
381.00 |
382.00 |
1.00 |
1.62 |
0.93 |
0.04 |
6.15 |
0.34 |
0.37 |
10.00* |
5.94 |
Fossilik: P-058 |
MQ-17-146 |
|
408.30 |
410.20 |
1.90 |
2.51 |
0.15 |
0.08 |
14.94 |
0.00** |
0.02 |
0.01 |
3.10 |
|
incl. |
408.30 |
408.90 |
0.60 |
4.70 |
0.40 |
0.18 |
30.89 |
BD |
0.03 |
0.03 |
5.99 |
|
and |
409.80 |
410.20 |
0.40 |
4.73 |
0.07 |
0.12 |
23.67 |
0.01 |
0.04 |
0.01 |
5.51 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
451.50 |
462.20 |
10.70 |
2.53 |
1.26 |
0.07 |
14.63 |
0.06 |
0.02 |
0.03 |
3.70 |
|
incl. |
452.50 |
456.00 |
3.50 |
4.97 |
2.30 |
0.13 |
28.26 |
0.09 |
0.04 |
0.07 |
7.10 |
|
and |
458.00 |
460.20 |
2.20 |
3.35 |
1.31 |
0.10 |
19.16 |
0.13 |
0.02 |
0.01 |
4.74 |
Fossilik: P-004 |
MQ-17-153 |
|
201.60 |
216.70 |
15.10 |
0.51 |
0.13 |
0.02 |
2.05 |
0.06 |
0.01 |
0.06 |
0.74 |
|
incl. |
208.00 |
216.00 |
8.00 |
0.76 |
0.18 |
0.03 |
3.18 |
0.08 |
0.02 |
0.07 |
1.07 |
P-013 SE |
MQ-17-140 |
|
247.35 |
268.20 |
20.85 |
0.65 |
0.47 |
0.02 |
2.77 |
0.11 |
0.05 |
0.22 |
1.13 |
|
incl. |
247.35 |
261.60 |
14.25 |
0.75 |
0.64 |
0.02 |
3.35 |
0.15 |
0.07 |
0.30 |
1.39 |
|
and |
267.00 |
268.20 |
1.20 |
1.65 |
0.12 |
0.04 |
5.61 |
0.05 |
0.09 |
0.05 |
2.00 |
|
|
|
|
|
|
|
|
|
|
|
|
|
MQ-17-142 |
|
298.00 |
303.70 |
5.70 |
0.50 |
0.51 |
0.02 |
2.48 |
0.07 |
0.06 |
0.66 |
1.13 |
Notes: Intervals represent core lengths, not necessarily true
widths*Ni EQ was calculated based on the following formula using
London Metal Exchange cash offer prices for Ni, Cu and Co on
January 12, 2018 and London Bullion Market Association metal prices
for Pt, Pt and Au on January 12, 2018 (PM) and assuming 100% metal
recoveries: *Ni EQ = Ni% + (Cu% x3.21/5.75) + (Co% x
34.25/5.75) + ((Pt g/t / 10000) x (991*14.5833/5.75)) + ((Pd g/t /
10000) x (1098 *14.5833/5.75)) + (Au g/t / 10000) x
(1326.80*14.5833/5.75)) (Metal prices are per pound and in
$US).
* Sample returned > 10 g/t and was cut to 10
g/t. ** Assay values for Pt is between 0.001 and 0.005 g/t, rounds
to “0”BD = Below Detection
Assays previously reported in news releases provided in the
text.
GEOLOGICAL SETTING, MAPPING AND 3D
MODELLING
In 2017, NAN geologists completed additional
detailed mapping in and adjacent to the IHC and Fossilik areas,
identifying new norite gossans and providing important structural
information. Downhole gyro and optical televiewer surveys
facilitated the collection of systematic subsurface structural data
and downhole physical properties surveys provided magnetic, gamma,
chargeability and resistivity data for comparison to surface
geophysical survey results. Surface and borehole geochemical
sampling results are being used to help identify melanorite
stratigraphy. SRK Consulting (Canada) Inc. continued to provide
structural geology support and is currently completing updated 3D
models for mineralized zones and the larger IHC and Fossilik
areas.
This work, which will ultimately help direct
exploration targeting in 2018, is leading to a better understanding
of the geometry of the mineralized zones; the effects of structural
offsets; the calibration of geophysical responses to sulphide
volume and content and; and the importance of melanorite as
sulphide hosts.
GEOPHYSICAL RESPONSE TO MASSIVE
SULPHIDE
Maniitsoq mineralization comprises disseminated,
blebby, net-textured, semi-massive and massive sulphides. Secondary
structural processes have affected primary sulphides resulting in
the formation of stringers, veins, fracture fillings and sulphide
breccia veins. The sulphide zones are commonly represented by
multiple discrete EM plates and this is interpreted to be due, at
least in part, to the remobilization and disruption of primary
magmatic sulphides. In 2017, large (13km2) IP surveys, were carried
out in the IHC and Fossilik areas to define the overall envelope of
existing zones and extensions of mineralized norite stratigraphy.
These surveys respond well to larger disseminated sulphide haloes
that surround the breccia style of mineralization
The EM method remains a critical workhorse, and
the application of this method in less deformed melanorite bodies
where the mineralization is connected will be a focus for
exploration in 2018.
MELANORITE FOCUS FOR FUTURE
EXPLORATION
The Maniitsoq mineralization hosted in
melanorite typically consists of disseminated sulphide containing a
higher grade discontinuous breccia style of semi-massive sulphide
mineralization. Previous work has established the very high nickel
concentrations in 100% sulphide that support the economic viability
of not just breccia styles of mineralization, but also the higher
grade disseminated sulphide style of mineralization. Work in 2017
has focused on the identification of the most extensive melanorite
intrusions using surface and borehole geochemistry, WV-3 satellite
imagery, and information from previous EM and IP surveys.
In 2018, NAN plans to implement a large
exploration program at Maniitsoq primarily comprising drilling and
geophysical surveys supported by the collection of geological,
geochemical and structural information and 3D modeling. These
efforts will be focussed on targeting the melanorite portions of
prioritized intrusions, such as Fossilik, which are viewed as
having the best potential to host economic accumulations of nickel
sulphides.
PROJECT PIPELINE
In the context of rising nickel prices and
positive developments in the electric vehicle market, NAN will look
to enhance shareholder value by aggressively expanding its nickel
sulphide project pipeline. NAN staff are proceeding with
compilation work on prospective geological environments related to
North American Archean cratonic margins where structural space
controls the development of mafic-ultramafic intrusions. The
objective of this work is to identify underexplored or unexplored
open system intrusions where high large zones of high grade
sulphide mineralization are controlled within the footprints of
very small intrusions.
Ongoing work continues to improve the geological
understanding and provide focus for exploration on the Post Creek
Property at the NE margin of the Sudbury Basin. The property lies
along the extension of the Whistle Offset dyke structure. Surface
mapping and petrology has identified pods of quartz diorite and
extensive domains of Sudbury Breccia along strike from the Whistle
Offset.
Technical Information; Qualified Person
The Company is not aware of any legal,
political, environmental or other risks that could materially
affect the potential development of the project other than those
set out in its annual information form filed on www.sedar.com.
Please see below under the heading "Cautionary Note Regarding
Forward-looking Statements" for further details regarding risks
facing the Company.
All technical information in this release has
been reviewed and approved by Peter C. Lightfoot, P.Geo. (Chief
Geologist) and Patricia Tirschmann, P.Geo (VP Exploration), who are
the Qualified Persons for the Company.
About North American Nickel
North American Nickel is a mineral exploration
company with 100% owned properties in Maniitsoq, Greenland and
Sudbury, Ontario.
The Maniitsoq property in Greenland is a Camp
scale project comprising 2,985 square km covering numerous
high-grade nickel-copper sulphide occurrences associated with
norite and other mafic-ultramafic intrusions of the Greenland
Norite Belt (GNB). The >75km-long belt is situated along, and
near, the southwest coast of Greenland accessible from the existing
Seqi deep water port with an all year round shipping season and
abundant hydro-electric potential.
The Post Creek/Halcyon property in Sudbury is
strategically located adjacent to the past producing Podolsky
copper-nickel-platinum group metal deposit of KGHM International
Ltd. The property lies along the extension of the Whistle Offset
dyke structure. Such geological structures host major Ni-Cu-PGM
deposits and producing mines within the Sudbury Camp.
Cautionary Note Regarding
Forward-looking Statements
This press release contains certain
"forward-looking statements" and "forward-looking information"
under applicable securities laws concerning the business,
operations and financial performance and condition of the Company.
Forward-looking statements and forward-looking information include,
but are not limited to, statements with respect to the success of
exploration activities; impact of mineralogy, estimation of mineral
resources at mineral projects of the Company; the future economics
of minerals including nickel and copper; synergies and financial
impact facilities; the benefits of the development potential of the
properties of the Company and currency exchange rate fluctuations.
Except for statements of historical fact relating to the Company,
certain information contained herein constitutes forward-looking
statements. Forward-looking statements are frequently characterized
by words such as "plan," "expect," "project," "intend," "believe,"
"anticipate," "estimate" and other similar words, or statements
that certain events or conditions "may" or "will" occur.
Forward-looking statements are based on the opinions and estimates
of management at the date the statements are made, and are based on
a number of assumptions and subject to a variety of risks and
uncertainties and other factors that could cause actual events or
results to differ materially from those projected in the
forward-looking statements. Many of these assumptions are based on
factors and events that are not within the control of the Company
and there is no assurance they will prove to be correct.
Factors that could cause actual results to vary
materially from results anticipated by such forward-looking
statements include variations in metal grades, changes in market
conditions, variations in recovery rates, risks relating to
international operations, fluctuating metal prices and currency
exchange rates, and other risks of the mining industry, including
but not limited to the failure of plant, equipment or processes to
operate as anticipated. The Company cautions that the foregoing
list of important factors is not exhaustive. Investors and others
who base themselves on forward-looking statements should carefully
consider the above factors as well as the uncertainties they
represent and the risk they entail. The Company believes that the
expectations reflected in those forward-looking statements are
reasonable, but no assurance can be given that these expectations
will prove to be correct and such forward-looking statements
included in this press release should not be unduly relied upon.
These statements speak only as of the date of this press release.
The Company undertakes no obligation to update forward-looking
statements if circumstances or management's estimates or opinions
should change except as required by applicable securities laws.
Although the Company has 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 anticipated, estimated or
intended. Statements concerning mineral reserve and resource
estimates may also be deemed to constitute forward-looking
statements to the extent they involve estimates of the
mineralization that will be encountered if the property is
developed.
Statements about the Company's future
expectations and all other statements in this press release other
than historical facts are "forward looking statements" within the
meaning of Section 27A of the Securities Act of 1933, Section 21E
of the Securities Exchange Act of 1934 and as that term defined in
the Private Litigation Reform Act of 1995. The Company intends that
such forward-looking statements be subject to the safe harbours
created thereby. Since these statements involve risks and
uncertainties and are subject to change at any time, the Company's
actual results may differ materially from the expected
results. For further information on the project,
please see National Instrument 43-101 (NI 43-101) technical report
prepared by SRK Consulting (Canada) Inc. (SRK) dated effective
March 17th, 2017, titled “Updated Independent Technical Report for
the Maniitsoq Nickel-Copper-Cobalt-PGM Project, Greenland”,
available under the Company's profile at www.sedar.com or at
www.northamericannickel.com.
ON BEHALF OF THE BOARD OF
DIRECTORS
Mark Fedikow PresidentNorth American Nickel
Inc.
For more information contact:
North American Nickel Inc.Jaclyn
RuptashCorporate Communications (604) 770-4334Toll free:
1-866-816-0118
Neither the TSX Venture Exchange nor its
Regulation Services Provider (as that term is defined in the
policies of the Exchange) accepts responsibility for the adequacy
or accuracy of this release.
A PDF accompanying this announcement is available
at http://resource.globenewswire.com/Resource/Download/e6dabace-2e88-4798-a6fe-7391e1e7db6e
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