VANCOUVER, BC, Oct. 17,
2023 /CNW/ - Nevada King Gold Corp. (TSXV:
NKG) (OTCQX: NKGFF) ("Nevada
King" or the "Company") is pleased to announce
assay results from five vertical 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. Highlight
holes reported today made a blind discovery 200m southwest of the Atlanta Pit in a previously
untested area within the southern extension of the West Atlanta
Graben Zone ("WAGZ") and are plotted in plan and along a new
Section 22-4N, the southernmost section line released to date at
Atlanta, (Figures 1-2).
Highlights:
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
AT23HG-37
|
170.7
|
285.1
|
114.3
|
1.89
|
2.8
|
Includes
|
222.6
|
227.1
|
27.06
|
4.60
|
17.9
|
AT23HG-34
|
135.7
|
231.7
|
96.0
|
2.15
|
5.1
|
Includes
|
202.7
|
231.7
|
27.4
|
4.50
|
13.3
|
AT23HG-35
|
134.1
|
155.5
|
21.3
|
3.42
|
9.3
|
Includes
|
147.9
|
154.0
|
6.1
|
10.39
|
22.0
|
AT23HG-36
|
143.3
|
175.3
|
32.0
|
1.10
|
2.7
|
Table 1.
Highlight holes released today. Mineralization occurs along
near-horizontal horizons with true mineralized thicknesses in
vertical holes estimated to be 85% to 100% of reported drill
intercept length.
|
- AT23HG-34 drilled along the West Atlanta Fault ("WAF")
and returned 2.15 g/t Au over 96m,
including 4.50 g/t Au over 27.4m.
AT23HG-37 was collared 36m west of
AT23HG-34 in Eureka Quartzite and drilled through 170m of barren, Ordovician-age quartzite before
intersecting Tertiary-age volcanic-hosted mineralization returning
1.89 g/t Au over 114.3m including
27.06 g/t Au over 4.6m.
- The presence of high-grade oxide mineralization beneath the
Eureka Quartzite in AT23HG-37 is considered a major development as
it indicates strong potential for extending the Atlanta resource zone southward into the South
Quartzite Ridge Target ("SQRT"). The SQRT is an undrilled
target area measuring approximately 1,000m long x 200m
wide that is contiguous to the Atlanta resource area and on trend with the
major faults that are interpreted as the primary plumbing for the
mineralizing fluids that deposited high-grade gold at Atlanta. These major feeder structures include
the WAF, the West Atlanta #1 and
#2 Faults, the Atlanta King Fault,
and the East Atlanta Fault, (see Figures 1 and 3 where fault traces
are plotted in plan).
- Previous explorers believed that gold mineralization terminated
at the easterly trending South Fault and saw no potential for a
southward continuation of mineralization along the WAF and into the
SQRT. As seen in Figure 2, the South Fault appears to have no
connection with gold mineralization and is instead most likely a
post-mineral structure, while the mineralized WAF continues south
into the SQRT. Past operators did conduct limited drilling to test
south of the South Fault, but utilized angle holes that generally
missed the mineralized horizon. As such, no historical drilling was
conducted south of Section 22-4N leaving the SQRT undrilled.
- CSAMT lines crossing the ridge show a resistivity low where the
SQRT is projected beneath the Eureka Quartzite extending several
hundred metres south of Section 22-4N, which may be correlative
with the mineralization hit in AT23HG-37 (Figures 3 and 4).
- As shown in Figure 2, the total width of mineralization across
Section 22-4N is 375m. Mineralization
to the west approaching the West Atlanta Fault #2 remains open and
untested. It is also evident in Figure 2 that a close spatial (if
not genetic) relationship exists between the rhyolitic intrusions
and gold mineralization hosted in adjacent silica breccia and
silicified volcanics. The main intrusive body is interpreted to
have migrated up along the WAF and spread both westward and
eastward along the Ordovician-Tertiary unconformity, localizing
gold mineralization within the intrusion and in adjacent silica
breccia and silicified volcanics. The stair-like arrangement of
fault blocks forming the AMFZ is very apparent.
Cal Herron, Exploration Manager
of Nevada King, stated,
"Nevada King's vertical holes
released today (averaging 2.05 g/t AuEq. over 105.2m thickness) paint a much brighter picture
of the potential of the SQRT than the historical angle holes
(averaging 1.64 g/t AuEq. over 26.3m
thickness) which mostly missed the mineralized horizon and
reaffirmed the historical misconception that the South Fault
terminated mineralization at Atlanta. Today's AT23HG-37 could prove a
significant development for resource potential at Atlanta should mineralization ultimately
continue southward along trend of the SQRT. Similar intersections
of gold mineralization found south of Section 22-4N would have a
marked impact on the resource potential at Atlanta by increasing mineralized tonnage and
reducing the overall strip ratio in a potential future mining
scenario. The Company is currently constructing drill pads south of
Section 22-4N to test the southern extension of the 100m thick, high-grade oxidized replacement
horizon found in today's drilling with an eye on tracing the
mineralization down to and possibly beyond the Atlanta Peak Fault
(Figure 3) along the axis of the Quartzite Ridge anticline. These
new results mark a major departure from the historical
interpretation at Atlanta, opening
up the potential for a larger mineralized system."




Discussion of South Quartzite
Ridge Target ("SQRT"):
The overall north-south trend to mineralization at Atlanta was recognized long before the deposit
was open-pitted, but exploration outside of the pit area largely
concentrated on chasing a potential northern extension. Potential
for a southern extension into the SQRT was considered to be
very low, largely because the massive, barren quartzite bounding
the southwestern side of the historical pit presented serious
challenges, namely lack of obvious mineralization and poor access.
Two historical angle holes about 350m
deep drilled under the western flank of the ridge hit Eureka
Quartzite and underlying Pogonip Limestone but no Au-Ag
mineralization, so efforts to test the ridge ceased by 1998. The
general consensus at that time was that mineralization at the
southern end of the pit was cut off by the South Fault (Figure 3)
and little if any potential existed for significant extension
southward. However, Nevada King's
2021 drilling directly south of the pit showed that mineralization
did indeed extend south of the South Fault, while the seven E-W
oriented CSAMT lines crossing the Quartzite Ridge in 2022 indicated
a prominent and persistent, sub-horizontal resistivity low
underlying the ridge's massive quartzite cap starting about
200m below the ridge crest (Figure
4).
Hole AT23HG-37 along Section 22-4N was sited on the northern end
of the SQRT in order to test for mineralization underneath the
quartzite. The hole collared in massive quartzite and drilled out
of largely barren quartzite and into mineralized felsic intrusive
tuff and rhyolite at 175m depth, with
mineralization continuing to 285m.
The contact between intrusive tuff and unaltered Pogonip Limestone
was hit at 430m depth. This
stratigraphic sequence is seen reflected in the resistivity section
shown in Figure 4 along CSAMT Line 09, which crosses the Quartzite
Ridge about 25m south of drill line
22-04N. Projecting the hit in AT23HG-37 southward onto Line 09, the
hole would penetrate the gold zone 40m west of the West Atlanta Fault. This same
stratigraphic profile is repeated southward past CSAMT Line 07
more than 400m south of AT23HG-37,
which now opens up a large area along the anticlinal axis in which
to pursue the type of thick mineralization penetrated in holes
AT23HG-37 and AT23HG-034, within a part of the property that has
never been previously drill-tested.
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
AT23HG-37
|
170.7
|
285.1
|
114.3
|
1.89
|
2.8
|
Includes
|
222.6
|
227.1
|
4.60
|
27.06
|
17.9
|
AT23HG-34
|
135.7
|
231.7
|
96.0
|
2.15
|
5.1
|
Includes
|
202.7
|
231.7
|
4.50
|
27.4
|
13.3
|
AT23HG-35
|
134.1
|
155.5
|
21.3
|
3.42
|
9.3
|
Includes
|
147.9
|
154.0
|
6.1
|
10.39
|
22.0
|
AT23HG-36
|
143.3
|
175.3
|
32.0
|
1.10
|
2.7
|
AT23ET-6
|
13.7
|
15.2
|
1.5
|
0.133
|
<0.5
|
Table 2. All
holes released today. Mineralization occurs along sub-horizontal
horizons generally dipping gently westward; true mineralized
thickness in vertical holes is between 85% and 95% of reported
drill intercept length.
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
AT22NS-81T*
|
101.8
|
129.9
|
28.0
|
2.90
|
8.1
|
Includes
|
123.2
|
128.5
|
5.3
|
10.73
|
21.4
|
AT22NS-83T*
|
96.6
|
128.7
|
32.0
|
3.19
|
14.6
|
Includes
|
110.4
|
127.1
|
16.8
|
5.35
|
24.1
|
AT22RC-1
|
48.8
|
88.4
|
39.6
|
0.55
|
4.5
|
AT22RC-13
|
0.0
|
19.8
|
19.8
|
0.99
|
7.4
|
AT22RC-16+
|
6.1
|
18.3
|
12.2
|
2.12
|
10.5
|
AT22RC-17
|
33.5
|
59.5
|
25.9
|
1.71
|
20.7
|
AT22RC-18
|
9.1
|
25.9
|
16.8
|
1.12
|
10.3
|
AT22RC-19
|
9.1
|
22.9
|
13.7
|
0.93
|
11.3
|
AT21-41A
|
38.1
|
61.0
|
22.9
|
2.17
|
33.7
|
AT21-42
|
9.1
|
36.6
|
27.4
|
0.79
|
3.3
|
AT21-43
|
10.7
|
29.0
|
18.3
|
0.95
|
10.0
|
AT21-43A
|
10.7
|
29.0
|
18.3
|
1.90
|
18.6
|
AT21-44
|
4.6
|
24.4
|
19.8
|
0.48
|
4.1
|
Table 3.
Previously reported holes used in previous releases along trace of
Section 22-4N. 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 is 85%
to 95% of the reported intercept length in vertical holes.
+Denotes holes that bottomed in mineralization.
*Denotes core hole.
|
Hole
No.
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au
(g/t)
|
Ag
(g/t)
|
KR98-2^
|
201.7
|
231.8
|
30.2
|
0.96
|
6.82
|
KR98-3^
|
202.9
|
219.1
|
16.2
|
0.83
|
0.9
|
KR98-4^
|
0.0
|
99.1
|
99.1
|
<0.02
|
<0.8
|
KR98-5^
|
0.0
|
138.7
|
138.7
|
<0.035
|
<1.0
|
KR97-14^
|
177.9
|
210.5
|
32.6
|
2.56
|
2.1
|
AR-20
|
114.3
|
115.9
|
1.5
|
0.27
|
0.1
|
AR-28^
|
130.4
|
146.7
|
16.3
|
0.87
|
6.2
|
AR-29
|
0.0
|
152.4
|
152.4
|
<0.003
|
<0.1
|
ARC-6
|
0.0
|
230.2
|
230.2
|
<0.003
|
<1.0
|
AC-5*
|
0.0
|
99.7
|
99.7
|
<0.003
|
<1.0
|
DHRI-11-10RC
|
108.2
|
129.6
|
21.3
|
1.75
|
10.6
|
DHRI-11-11RC^
|
88.3
|
111.4
|
23.1
|
1.07
|
5.1
|
DHRI-11-10C*
|
74.7
|
114.3
|
39.6
|
1.75
|
23.1
|
Table
4. Historical holes used in Section 22-4N. KR97 and
KR98 series holes were drilled by Kinross in 1997 and 1998. AR,
ARC, and AC series holes were drilled by Goldfields in 1991.
DHRI-11 series holes were drilled by Meadow Bay in 2011. True
thickness of gold mineralization interpreted in today's
release is 85% to 95% of the reported intercept length in vertical
holes. ^Denotes angle hole. *Denotes core
hole.
|
Operator
|
West Atlanta
Graben
|
Atlanta Mine Fault
Zone
|
|
No. of
Holes
|
Average AuEq.
(g/t)
|
Average
Thickness (m)
|
No. of
Holes
|
Average Au Eq
. (g/t)
|
Average
Thickness (m)
|
Nevada
King
|
2
|
2.05
|
105.2
|
15
|
1.76
|
23.2
|
Historical
|
3
|
1.64
|
26.3
|
4
|
1.61
|
25.0
|
Table 5.
Comparison of Nevada King and historical drill results along
section line 22-4N, using weighted averages. Gold equivalents
calculated using Au/Ag prices of $1,833/oz and $21.59/oz,
respectively, (Oct 7, 2023 $US spot prices).
|
QA/QC Protocols
All Reverse Circulation (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 mutli-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. 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 Ag
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 6. 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.

View original content to download
multimedia:https://www.prnewswire.com/news-releases/nevada-king-makes-blind-discovery-intercepting-1-89-gt-au-over-114-3m-and-2-15-gt-au-over-96-0m-200m-south-of-the-atlanta-pit-in-the-south-quartzite-ridge-target-301958312.html
SOURCE Nevada King Gold Corp.