Nevada KING Makes Blind Discovery Intercepting 1.89 G/T Au over 114.3M and 2.15 G/T Au over 96.0M 200M South of the Atlanta Pit IN the 'South Quartzite Ridge Target'
NEVADA KING MAKES BLIND DISCOVERY INTERCEPTING 1.89 G/T AU
OVER 114.3M AND 2.15 G/T AU OVER 96.0M 200M SOUTH OF THE
ATLANTA PIT IN THE 'SOUTH QUARTZITE RIDGE TARGET'
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."
Figure 1. Location map for holes reported in this news release along drill Section 22-4N relative to the perimeter of the historical Atlanta Pit and footprint of the
Gustavson 2020 NI 43-101 resource. Shallow drillholes on the mine dumps have been removed from the plot for clarity. (CNW Group/Nevada King Gold Corp.)
Figure 2. New cross Section 22-4N looking north across WAF that divides AMFZ target on east from WAGZ target on west. Along the AMFZ Au/Ag mineralization
is largely hosted within a silica breccia horizon developed on top the Paleozoic dolomite and quartzite units, whereas mineralization within the WAGZ is largely
hosted within volcanic tuff and sediments above the Paleozoic basement. Note the close spatial relationship between mineralization and the rhyolitic intrusion in
both target areas. (CNW Group/Nevada King Gold Corp.)
Figure 3. Generalized geologic map of SQRT area showing CSAMT resistivity high over the Quartzite Ridge and flanking resistivity lows related to felsic tuff,
rhyolite, and dacite intrusions that are spatially related to gold mineralization. Target is completely covered by massive quartzite and is structurally dominated by a
gently north-plunging open anticline intruded along its axis by northerly-trending rhyolitic and dacitic tuff dikes. The target is untested by previous drilling. (CNW
Group/Nevada King Gold Corp.)
Figure 4. Portion of CSAMT resistivity section line 09 (not to be confused with previously released drill Section22-9N) looking north across SQRT, showing drill
hole intercepts & major structures. Blue color denotes high resistivity zones (quartzite, dolomite, & strong silicification), while hot colors denote low resistivity
zones (volcanics, intrusives, & adjacent altered sediments). Black hatched area indicates southward projection of gold mineralized zone from drill Section 22-4N.
Spacing on grid is 100m. (CNW Group/Nevada King Gold Corp.)
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.
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For further information:
Collin Kettell at [email protected] or (845) 535-1486.
CO: Nevada King Gold Corp.
CNW 07:30e 17-OCT-23