North American Nickel Inc. (TSX VENTURE:NAN)
(OTCBB:WSCRF) (CUSIP:65704T 108) (the "
Company")
is pleased to report that assays have been received from seven
drill holes and one drill hole extension completed to test targets
at Fossilik and the Imiak Hill Complex (IHC) on the Company’s 100%
owned Maniitsoq nickel-copper-cobalt-PGM sulphide project in
southwest Greenland. Hole MQ-17-153 intersected multiple zones with
elevated nickel values at the P-004 target area within the large
Fossilik intrusion.
Drilling, mapping and surface sampling continue
to expand and discover new mineralization in both the Fossilik and
IHC areas. Data synthesis is providing a deeper understanding of
the Maniitsoq mineral system and will guide efforts in 2018 to
locate larger volumes of higher grade mineralization.
Highlights include:
- MQ-17-153:
- 15.10m @ 0.51% Ni, 0.13% Cu, 0.02% Co and 0.13 g/t Pt+Pd+Au
including
- 8.00m @ 0.76% Ni, 0.18% Cu, 0.03% Co and 0.17 g/t Pt+Pd+Au
- Moderate conductance off-hole borehole electromagnetic (BHEM)
anomalies are correlated with mineralization intersection in
MQ-17-153.
- Surface sampling immediately east of the Fossilik intrusion at
the P-246 target returned 2.04% Ni, 0.51% Cu, 0.12% Co and 0.30 g/t
Pt+Pd+Au in a plugger sample.
- Surface sampling returned anomalous nickel values of up to
0.79% nickel and 0.56% copper at several new locations peripheral
to the IHC including at the large G-025 norite intrusion.
- Melanorites have been identified as an important host to high
nickel tenor disseminated sulphide mineralization at Fossilik and
associated with the IHC. The larger melanorite bodies have the
capacity to host thicker zones of breccia and semi-massive
sulphides, potentially in the keels of the intrusions.
NAN CEO, Keith Morrison, commented: “Fossilik
encompasses the largest mineralized norite body identified at
Maniitsoq to date. It is important to consider the MQ-17-153 assay
results at P-004 in combination with drilling results at P-058 and
P-059 and the wide areas of surface nickel sulphide mineralization
as being cumulatively representative of the nickel bearing capacity
of the Fossilik intrusion. Further evaluation of this area will be
a priority for NAN in our 2018 exploration program.”
During the 2017 exploration program, 23 drill
holes totalling 8,767 metres were completed to test mineralized
zones and geophysical targets in the IHC, Fossilik and P-013 SE
areas within the Greenland Norite Belt (Figure 1). This release,
which concludes the 2017 reporting, summarizes results for seven
holes totalling 2,679 metres, as well as for the extension of hole
MQ-17-135 at Mikissoq and the 2017 surface sampling program. Drill
collar information and a summary of assays are provided in Tables 1
and 2 respectively. Table 3 lists the highlights of the surface
sampling program. Plan maps for the Fossilik and IHC areas are
provided in Figure 2 and 3, respectively. Figures may be viewed
using the link provided at the end of this release.
Further details are given below.
Table 1: Drill Collar
Information
HoleNumber |
UTM East |
UTM North |
Elevation(m) |
Length(m) |
Azimuth |
Dip |
Target |
Imiak Hill Complex |
|
MQ-17-147 |
477503 |
7258315 |
357 |
754.00 |
116 |
-61 |
IP Target |
MQ-17-149 |
478986 |
7256689 |
574 |
170.60 |
80 |
-56 |
G-004 |
MQ-17-150 |
478567 |
7257150 |
588 |
423.00 |
66 |
-68 |
IP Target |
MQ-17-154 |
477998 |
7257310 |
536 |
465.40 |
50 |
-67 |
IP Target |
Fossilik Area |
MQ-17-153 |
474463 |
7248748 |
658 |
437.00 |
26 |
-64 |
P-004 |
MQ-17-155 |
474089 |
7249769 |
548 |
292.05 |
124 |
-53 |
Fossilik I |
MQ-17-156 |
476055 |
7248493 |
514 |
137.00 |
8 |
-60 |
P-246 |
Note: Collar coordinates in UTM WGS84 Zone
22N
Table 2: Assay Results
HoleNumber |
|
From(m) |
To (m) |
CoreLength(m) |
Ni % |
Cu % |
Co % |
S % |
Pt g/t |
Pd g/t |
Au g/t |
|
Fossilik - Target P-004 |
MQ-17-153 |
|
69.10 |
88.20 |
19.10 |
0.22 |
0.06 |
0.01 |
0.92 |
0.02 |
0.00* |
0.03 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
150.00 |
164.00 |
14.00 |
0.14 |
0.03 |
0.01 |
0.39 |
0.02 |
0.00* |
0.02 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
182.00 |
193.90 |
11.90 |
0.18 |
0.04 |
0.01 |
0.59 |
0.02 |
0.00* |
0.02 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
201.60 |
216.70 |
15.10 |
0.51 |
0.13 |
0.02 |
2.05 |
0.06 |
0.01 |
0.06 |
|
incl. |
208.00 |
216.00 |
8.00 |
0.76 |
0.18 |
0.03 |
3.18 |
0.08 |
0.02 |
0.07 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
246.20 |
246.90 |
0.70 |
0.53 |
0.13 |
0.03 |
2.43 |
0.07 |
0.02 |
0.05 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
252.00 |
252.65 |
0.65 |
0.65 |
0.09 |
0.02 |
2.49 |
0.06 |
0.02 |
0.03 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
388.10 |
405.20 |
17.10 |
0.35 |
0.10 |
0.01 |
1.37 |
0.05 |
0.01 |
0.03 |
No significant assays for holes MQ-17-147,
MQ-17-149, MQ-17-150, MQ-17-154, MQ-17-155, MQ-17-156 &
MQ-17-135 hole extension (495 to 783 metres). |
Note: Intervals represent core lengths, not
necessarily true widths.* Assay value for Pd is between 0.001 and
0.005 g/t, rounds to “0”.
Table 3: Highlights of Surface
Sampling
SampleNo. |
Area |
UTMEast |
UTMNorth |
Ni % |
Cu % |
Co % |
S % |
Pt g/t |
Pd g/t |
Au g/t |
|
D06013 |
IHC |
476142 |
7256553 |
0.42 |
0.14 |
0.03 |
3.73 |
0.01 |
0.01 |
0.01 |
D06018 |
G-025 |
473474 |
7256402 |
0.41 |
0.20 |
0.02 |
2.08 |
0.36 |
0.22 |
0.14 |
D06019 |
G-025 |
473384 |
7256594 |
0.56 |
0.56 |
0.03 |
2.87 |
0.35 |
0.21 |
0.13 |
D06022 |
G-025 |
472562 |
7255460 |
0.79 |
0.42 |
0.04 |
3.50 |
0.09 |
0.04 |
0.12 |
D06038 |
G-018 |
475385 |
7256138 |
0.55 |
0.41 |
0.02 |
2.70 |
0.03 |
0.02 |
0.07 |
D06040 |
P-246 |
475914 |
7248518 |
2.04 |
0.51 |
0.12 |
18.70 |
0.10 |
0.04 |
0.16 |
D06063 |
P-246 |
475688 |
7248214 |
1.08 |
0.45 |
0.10 |
12.20 |
0.11 |
0.03 |
0.05 |
D06078 |
IHC |
477754 |
7255975 |
0.48 |
0.27 |
0.03 |
2.93 |
0.11 |
0.07 |
0.03 |
All samples represent grab samples with the exception of the
sample D06040 which was a shallow plugger sample.
Fossilik
Figure 2
The Fossilik area is located in the central
portion of the Greenland Norite belt and comprises several
mineralized norite intrusions which host numerous surface gossans
and significant zones of nickel copper sulphides intersected in
drilling (see Figure 2). The central of these is the four kilometre
long Fossilik intrusion where recent drilling completed by NAN has
intersected additional high grade nickel copper sulphides (2.53%
nickel and 1.26% copper over 10.7 metres) and has extended the
P-058 zone to a vertical depth of 650 metres (see News Release
dated November 23, 2017).
Three holes totaling 866 metres were completed
to test surface induced polarization (IP) and EM anomalies at the
P-004, P-246 and Fossilik I targets (see Figure 2).
Hole MQ-17-153, drilled at P-004 within the
Fossilik intrusion, intersected a number of zones of norite-hosted
mineralization which returned anomalous nickel values (see Table
1). The best results included 0.51% nickel and 0.13% copper over
15.10 metres from 201.6 to 216.7 metres including 0.76% nickel and
0.18% copper over 8.0 meters. Borehole EM surveys identified
multiple small moderate conductance off-hole anomalies, several of
which are interpreted to correlate with mineralization intersected
at 200 and 400 metres downhole. Structural analysis and 3D modeling
is in progress to be help determine the relationship of these new
intersections and BHEM anomalies to previous drilling and
geophysical results at P-004.
Holes MQ-17-155 and MQ-17-156 were drilled at
the Fossilik I and P-246 target areas, respectively. Both holes
intersected norite but did not intersect any significant
mineralization. Weak to moderate off-hole BHEM anomalies were
detected in borehole surveys. Surface sampling at P-246 returned
highly anomalous values of up to 2.04% nickel, 0.51% copper, 0.12%
cobalt and 0.30 g/t Pt+Pd+Au.
The Fossilik area hosts one of the largest known
volumes of norite on the Maniitsoq Property and additional
mineralization continues to be discovered. To date, the Fossilik
intrusion is only partially explored and additional sampling,
geophysics and drilling are planned for 2018.
Imiak Hill Complex and Surrounding
Area
Figure 3
The Imiak Hill Complex is located 8 km north of
Fossilik and comprises the Mikissoq, Imiak Hill and Spotty Hill
sulphide zones. A number of additional mineralized norite
intrusions occur peripheral to the IHC, particularly to the
west.
Four holes (MQ-17-147, 149, 150 and 154)
totaling 1,813 metres were completed to test surface IP anomalies
at the IHC but did not return significant assays (see Figure 3).
Mapping and sampling outward from the IHC identified new gossans
which returned values of up to 0.79% nickel and 0.56% copper
including several samples from the large G-025 norite intrusion
located 4 kilometres west of the IHC.
Comment on Maniitsoq Mineralization and Future
Plans
Systematic analysis of geochemical data
indicates that melanorites (> 12.5 wt MgO) are an important host
to disseminated sulphide mineralization at both Fossilik and the
IHC and this rock type also hosts thick zones of breccia and
semi-massive sulphides. The melanorite keels of large mineralized
intrusions such as Fossilik and target G-025 therefore represent an
important geological environment to explore for large tonnage, high
grade mineralization.
In addition, the Maniitsoq nickel sulphide
mineralization consistently displays very high nickel tenors
(percent nickel re-calculated to 100% sulphides), typically ranging
from 5 to 10.5 wt % making near surface disseminated sulphide zones
viable exploration targets in this environment.
Exploration in 2018 is expected to focus on both
breccia-massive sulphides, potentially located in intrusion keels,
as well near surface disseminated sulphide targets in order to
locate larger volumes of sulphides and more quickly achieve the
Company’s tonnage/size goals for the project.
Quality Control
The drilling was completed by Cabo Drilling Corp
(Canada) utilizing two Atlas Copco S2 diamond drill rigs.
Additionally, drilling completed in September included a Helí 1500
Marcotte drill rig sourced from Arctic Core Drilling A/S
(Greenland) and manned by a drill crew from Forage-M3 Drilling
(Canada). Drill core samples (36.5 mm BQ and 47.6 mm NQ) are cut in
half by a diamond saw on site. Half of the core is retained
for reference purposes. Samples are generally 1.0 to 1.5
metre intervals or less at the discretion of the site geologists.
Sample preparation is completed at the GeoLAB Greenland ApS
preparation lab in Nuuk, Greenland. Sample pulps are sent by
air to the MS Analytical laboratory in Langley, BC, Canada.
Blank samples and commercially prepared and certified Ni sulphide
analytical control standards with a range of grades are inserted in
every batch of 20 drill core samples or a minimum of one per sample
batch. Blank samples and/or commercially prepared and
certified Ni sulphide analytical control standards are also
inserted into every batch of surface samples. Analyses for Ni, Cu
and Co are completed using a sodium peroxide fusion preparation and
ICP-ES finish (PER-700). Analyses for Pt, Pd, and Au are by
fire assay (30 grams nominal sample weight) with an ICP-AES finish
(FAS-113).
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 Patricia Tirschmann, P.Geo, who is
the Qualified Person for the Company and Vice President
Exploration, North American Nickel Inc.
About North American NickelNorth 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/baf04381-4ba1-4d6a-9556-45438e926975
North American Nickel (TSXV:NAN)
Graphique Historique de l'Action
De Nov 2024 à Déc 2024
North American Nickel (TSXV:NAN)
Graphique Historique de l'Action
De Déc 2023 à Déc 2024