VANCOUVER, BC, June 5, 2024
/CNW/ - Nevada King Gold Corp. (TSXV: NKG) (OTCQX:
NKGFF) ("Nevada King" or
the "Company") is pleased to announce assay results from one
metallurgical core hole and two reverse circulation ("RC")
holes recently completed at its Atlanta Gold Mine Project located
264km northeast of Las Vegas,
Nevada, in the prolific Battle Mountain Trend. Today's holes
are plotted in plan and along updated Section 23-7N(4), (Figures
1-2).
Highlights:
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Zone
|
AT23NS-54C+
|
160.1
|
190.9
|
30.7
|
6.14
|
79.3
|
WAF
|
includes
|
162.3
|
188.1
|
25.8
|
6.94
|
90.5
|
WAF
|
AT24NS-174B^
|
109.8
|
158.5
|
48.8
|
3.08
|
33.2
|
WAF
|
includes
|
118.9
|
125.0
|
6.1
|
7.00
|
75.5
|
WAF
|
AT24NS-174C^
|
103.7
|
138.7
|
35.1
|
4.15
|
47.4
|
WAF
|
includes
|
105.2
|
111.3
|
6.1
|
11.06
|
110
|
WAF
|
Table 1. Holes released today. Mineralization occurs
along the northerly-trending West Atlanta Fault within an
intrusive breccia zone dipping 60o to
70o west. True mineralized thickness estimated to be 35%
to 45% of reported intercept length.
+Denotes core hole. ^Denotes steep angle hole
(-83o dip).
|
- Core hole AT23NS-54C intercepted 6.14 g/t Au and 79.3 g/t Ag
over 30.7m and was sited to
collect mineralized silica breccia occurring along the West Atlanta
Fault ("WAF") for the ongoing Phase II metallurgical
testwork program. The WAF forms the fault boundary between the
Atlanta Mine Fault Zone ("AMFZ") on the east and the West
Atlanta Graben Zone ("WAGZ") on the west.
- Angle holes AT24NS-174B (3.08 g/t Au over 48.8m) and AT24NS-174C (4.15 g/t Au over
35.1m) were designed to infill a
gap in drill coverage along the western side of the AMFZ and also
track the southern extension of the northerly-trending high-grade
intrusive contact in the hanging wall of the WAF that was
intercepted in adjacent holes (see Table 2 below) along lines both
north and south of Section 23-7N(4) as shown in Figure 3.
- These closely-spaced angle holes clearly demonstrate a
consistent 60o to 70o west dip to this
mineralized zone that likely served as the Atlanta deposit's main hydrothermal flue (or
feeder) along the WAF. The zone is between 15m and 20m true
thickness and is bounded on the east by massive Eureka Quartzite.
Mineralization is hosted within strongly silicified fault and
hydrothermal breccias mixed with silicified volcanics and narrow
intrusive dikes. The highest gold grades tend to occur along
contacts with silicified porphyritic rhyolite dikes.
- As shown in Figure 3, this high-grade, intrusive dominated zone
looks to vear NW and pinch out but remains open to the south
where it appears to widen and curve southwestward and possibly
connect to more high-grade intercepts along Section 22-4N.
- Referring to Figure 2, gold mineralization thickens and
flattens moving westward and eastward from this WAF feeder zone as
the hydrothermal fluids migrated laterally into receptive volcanic
and intrusive host rocks within the adjacent WAGZ as well as along
the low-angle unconformity separating younger volcanics and
intrusions from underlying Paleozoic basement rocks in the AMFZ.
The silica breccia unit hosting most of the mineralization along
the fault was originally interpreted as having formed along the
sub-horizontal unconformity and subsequently down dropped in a
step-like manner across the fault zone. However, recent re-logging
of drill data revealed that much of the silica breccia within this
steeply dipping structure is intensely silicified, brecciated
rhyolitic intrusive rock as opposed to strongly silicified
dolomitic rock underneath the unconformity. Trace element
enrichment in chromium coupled with depletion of titanium and
magnesium within the silica breccia confirm a largely rhyolitic
host rock (prolith). Understanding this direct relationship between
rhyolitic intrusions and high-grade gold mineralization could be a
key indicator for understanding and potentially targeting gold
distribution throughout the Atlanta district.
Cal Herron, Exploration Manager
of Nevada King, stated, "The
Atlanta gold/silver deposit
evolved within a complex geological environment replete with
long-lived faulting, caldera resurgence, multiple intrusive events,
and numerous mineralizing events. It is this complexity and
interplay of recurring events over a long period of time that can
allow for the formation of large gold systems. The Company is in
the midst of a relogging program with a close focus on trace
element geochemical patterns to identify protoliths within strongly
altered/mineralized zones, which will allow us to further refine
our geologic model. By focusing on stable trace elements that
remain relatively immobile during hydrothermal alteration, we have
been able to differentiate protolith types within the silica
breccia unit to more accurately identify critical structures and
lithotypes responsible for gold mineralization. For example, the
resistate metals suite consisting of titanium-chromium-magnesium
does a good job of differentiating dacitic, rhyolitic, quartzite,
and dolomite protoliths; while the hydrothermal suite
gold-arsenic-antimony-molybdenum-thallium-barium works well for
identifying hydrothermal flues/feeders and preferred fluid pathways
hosting higher gold grades. With this understanding in place, we
now see opportunities for applying this knowledge to unlock the
potential of Atlanta both at the
district scale as well as within the immediate vicinity of the
Atlanta deposit, such as at the
South Quartzite Ridge Target, the North Extension Target, the East
Ridge Target, and potentially to depth."
Line
#
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
9
|
AT23NS-133E*
|
122.0
|
202.7
|
80.8
|
1.99
|
|
includes
|
196.6
|
198.2
|
1.5
|
10.25
|
8
|
AT22NS-053
|
157
|
224.1
|
67.1
|
2.88
|
|
includes
|
205.8
|
218.0
|
12.2
|
11.12
|
8
|
AT23NS-174*
|
117.4
|
186.0
|
68.6
|
6.90
|
|
includes
|
166.2
|
176.8
|
10.7
|
19.20
|
8
|
AT23NS-174A*
|
118.9
|
196.6
|
77.7
|
4.90
|
|
includes
|
169.2
|
172.3
|
3.0
|
19.35
|
8
|
AT23NS-133F*
|
117.4
|
199.7
|
82.3
|
6.55
|
|
includes
|
184.5
|
196.6
|
12.2
|
26.71
|
7
|
AT24NS-174B*
|
109.8
|
158.5
|
48.8
|
3.08
|
|
includes
|
118.9
|
125.0
|
6.1
|
7.00
|
7
|
AT24NS-174C*
|
103.7
|
138.7
|
35.1
|
4.15
|
|
includes
|
105.2
|
111.3
|
6.1
|
11.06
|
6
|
AT22NS-68
|
134.0
|
163.1
|
29.1
|
4.03
|
|
includes
|
157.0
|
160.1
|
3.1
|
10.03
|
6
|
AT23NS-131C*
|
132.6
|
172.3
|
39.6
|
4.91
|
|
includes
|
144.8
|
154.0
|
9.2
|
12.94
|
Table 2. Mineralized intervals in RC holes defining a
northerly-trending high-grade zone along the hanging wall side of
the steeply west-dipping West Atlanta Fault ("WAF"). True
mineralized thickness estimated to be between 25% and 50%
of reported intercept length and is dependent on hole dip and
location of entry point into the WAF structure. *Denotes
angle hole.
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
Zone
|
AT23WS-47
|
219.5
|
332.3
|
112.8
|
0.58
|
3.2
|
WAGZ
|
AT23WS-48
|
207.3
|
346.0
|
138.7
|
0.32
|
5.3
|
WAGZ
|
AT23HG-38
|
214.9
|
329.3
|
114.3
|
1.43
|
16.5
|
WAGZ
|
AT23NS-131C*
|
132.6
|
172.3
|
39.6
|
4.91
|
41.4
|
WAF
|
AT23NS-133A*
|
99.1
|
123.5
|
24.4
|
2.33
|
24.6
|
AMFZ
|
AT23NS-133B*
|
99.1
|
120.4
|
21.3
|
2.99
|
22.8
|
AMFZ
|
AT23NS-133D*
|
73.2
|
97.6
|
24.4
|
2.25
|
23.3
|
AMFZ
|
AT23WS-36
|
242.4
|
335.4
|
93.0
|
0.54
|
7.6
|
WAGZ
|
AT22HG-6
|
189.0
|
256.1
|
67.1
|
1.34
|
6.4
|
WAGZ
|
AT23HG-23
|
227.1
|
317.1
|
89.9
|
0.57
|
11.5
|
WAGZ
|
AT23NS-125*
|
74.7
|
109.8
|
35.1
|
1.26
|
31.9
|
AMFZ
|
AT22HG-5
|
186.0
|
279.0
|
93.0
|
1.14
|
2.1
|
WAGZ
|
AT22HG-3T
|
170.4
|
285.4
|
93.6
|
2.18
|
17.1
|
WAGZ
|
AT22HG-4
|
175.3
|
240.9
|
41.2
|
1.92
|
22.7
|
WAGZ
|
AT22NS-68
|
134.1
|
163.1
|
29.0
|
4.03
|
21.2
|
WAF
|
AT22NS-54
|
170.7
|
216.5
|
45.7
|
4.21
|
79.6
|
WAF
|
AT22NS-56A
|
93.0
|
106.7
|
13.7
|
1.88
|
38.5
|
AMFZ
|
AT22NS-76
|
70.1
|
100.6
|
30.5
|
2.39
|
41.5
|
AMFZ
|
AT22NS-73
|
22.9
|
103.7
|
80.8
|
2.31
|
47.4
|
AMFZ
|
AT21-68C+
|
99.1
|
120.3
|
21.2
|
3.28
|
34.4
|
WAF
|
Table
3. Previously reported holes used along updated
Section 22-7N(3). AT22 series holes were drilled by Nevada King
in 2022 and the AT21 series holes were drilled in 2021. True
thickness of gold mineralization interpreted in today's release
for holes penetrating the WAF is 30% to 45% of the reported
intercept length. True thickness in holes penetrating the AMFZ
and WAGZ is interpreted to be 90% to 100% of the reported
intercept length in vertical holes and 75% to 90% of reported
intercept length in angle holes. +Denotes core hole. *Denotes angle
hole.
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
AR-21
|
240.8
|
304.8
|
64
|
0.39
|
4.21
|
AR-19
|
228.6
|
304.8
|
76.2
|
0.82
|
3.52
|
KR97-9*
|
175.3
|
210.4
|
35.1
|
4.81
|
25.2
|
includes
|
196.6
|
201.2
|
4.6
|
21.83
|
27.8
|
DHRI-11-6C+
|
227.1
|
295.1
|
68
|
1.11
|
15.7
|
DHRI-11-1C+*
|
74.7
|
97.5
|
22.8
|
1.90
|
19.7
|
Table
4. Historical holes used in updated Section
22-7N(3). AR series holes were drilled by Goldfields in 1991. KR
series holes were drilled by Kinross in 1997. DHRI series
holes were drilled by Meadow Bay in 2011. True thickness of
gold mineralization interpreted in today's release is 90% to
100% of the reported intercept length in vertical holes.
True mineralized thickness in angle holes estimated to be 75%
to 90% of reported intercept length. +Denotes core hole. *Denotes
angle hole.
|
QAQC Protocols
All RC samples from the Atlanta Project are split at the drill
site and placed in cloth and plastic bags utilizing a nominal 2kg
sample weight. CRF standards, blanks, and duplicates are inserted
into the sample stream on-site on a one-in-twenty sample basis,
meaning all three inserts are included in each 20-sample group.
Samples are shipped by a local contractor in large sample shipping
crates directly to American Assay Lab in Reno, Nevada, with full custody being
maintained at all times. At American Assay Lab, samples were
weighed then crushed to 75% passing 2mm and pulverized to 85%
passing 75 microns in order to produce a 300g pulverized split.
Prepared samples are initially run using a four acid + boric acid
digestion process and conventional multi-element ICP-OES analysis.
Gold assays are initially run using 30-gram samples by lead fire
assay with an OES finish to a 0.003 ppm detection limit, with
samples greater than 10 ppm finished gravimetrically. Silver
samples that run greater than 100ppm are also finished
gravimetrically. Every sample is also run through a cyanide leach
for gold with an ICP-OES finish. The QA/QC procedure involves
regular submission of Certified Analytical Standards and
property-specific duplicates.
Qualified Person
The scientific and technical information in this news release
has been reviewed and approved by Calvin R.
Herron, P.Geo., who is a Qualified Person as defined by
National Instrument 43-101 ("NI 43-101").
About Nevada King Gold Corp.
Nevada King is the third largest
mineral claim holder in the State of
Nevada, behind Nevada Gold
Mines (Barrick/Newmont) and Kinross
Gold. Starting in 2016, the Company has staked large project
areas hosting significant historical exploration work along the
Battle Mountain trend located
close to current or former producing gold mines. These project
areas were initially targeted based on their potential for hosting
multi-million-ounce gold deposits and were subsequently staked
following a detailed geological evaluation. District-scale projects
in Nevada King's portfolio include
(1) the 100% owned Atlanta Mine, located 100km southeast of
Ely, (2) the Lewis and Horse
Mountain-Mill Creek projects, both located between Nevada Gold Mines' large Phoenix and Pipeline mines, and (3) the Iron
Point project, located 35km east of Winnemucca, Nevada.
The Atlanta Mine is a historical gold-silver producer with a NI
43-101 compliant pit-constrained resource of 460,000 oz Au in the
measured and indicated category (11.0M tonnes at 1.3 g/t) plus an inferred
resource of 142,000 oz Au (5.3M
tonnes at 0.83 g/t). See the NI 43-101 Technical Report on
Resources titled "Atlanta Property, Lincoln County, NV" with an effective date of
October 6, 2020, and a report date of
December 22, 2020, as prepared by
Gustavson Associates and filed under the Company's profile on
SEDAR+ (www.sedarplus.ca).
Resource
Category
|
Tonnes
(000s)
|
Au Grade
(ppm)
|
Contained Au
Oz
|
Ag Grade
(ppm)
|
Contained Au
Oz
|
Measured
|
4,130
|
1.51
|
200,000
|
14.0
|
1,860,000
|
Indicated
|
6,910
|
1.17
|
260,000
|
10.6
|
2,360,000
|
Measured +
Indicated
|
11,000
|
1.30
|
460,000
|
11.9
|
4,220,000
|
Inferred
|
5,310
|
0.83
|
142,000
|
7.3
|
1,240,000
|
Table 5. NI
43-101 Mineral Resources at the Atlanta Mine
|
Please see the Company's website at www.nevadaking.ca.
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 release.
Cautionary Statements Regarding Forward Looking
Information
This news release contains certain "forward-looking
information" and "forward-looking statements" (collectively
"forward-looking statements") within the meaning of applicable
securities legislation. All statements, other than statements of
historical fact, included herein, without limitation, statements
relating the future operations and activities of Nevada King, are forward-looking statements.
Forward-looking statements are frequently, but not always,
identified by words such as "expects", "anticipates", "believes",
"intends", "estimates", "potential", "possible", and similar
expressions, or statements that events, conditions, or results
"will", "may", "could", or "should" occur or be achieved.
Forward-looking statements in this news release relate to, among
other things, the Company's exploration plans and the Company's
ability to potentially expand mineral resources and the impact
thereon. There can be no assurance that such statements will prove
to be accurate, and actual results and future events could differ
materially from those anticipated in such statements.
Forward-looking statements reflect the beliefs, opinions and
projections on the date the statements are made and are based upon
a number of assumptions and estimates that, while considered
reasonable by Nevada King, are
inherently subject to significant business, economic, competitive,
political and social uncertainties and contingencies. Many factors,
both known and unknown, could cause actual results, performance or
achievements to be materially different from the results,
performance or achievements that are or may be expressed or implied
by such forward-looking statements and the parties have made
assumptions and estimates based on or related to many of these
factors. Such factors include, without limitation, the ability to
complete proposed exploration work, the results of exploration,
continued availability of capital, and changes in general economic,
market and business conditions. Readers should not place undue
reliance on the forward-looking statements and information
contained in this news release concerning these items. Nevada King does not assume any obligation to
update the forward-looking statements of beliefs, opinions,
projections, or other factors, should they change, except as
required by applicable securities laws.
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