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Eskay Mining Encounters 1.51 Gpt Au and 25.39 Gpt Ag Over 43.1m and 2.84 Gpt Au and 22.17 Gpt Ag Over 16.4m in Extensional Drilling at the TV Deposit, Consolidated Eskay Project, Golden Triangle, BC

Eskay Mining Encounters 1.51 Gpt Au and 25.39 Gpt Ag Over 43.1m and 2.84 Gpt Au and 22.17 Gpt Ag Over 16.4m in Extensional Drilling at the TV Deposit, Consolidated Eskay Project, Golden Triangle, BC

愛斯凱礦業在不列顛哥倫比亞省金三角市的金三角合併埃斯凱項目(Eskay)合併 Eskay 項目(Eskay)項目遭遇了 1.51 Gpt Au 和 25.39 Gpt Ag,以及 22.17 Gpt Ag 公司遭遇了 1.51 Gpt Ag
Accesswire ·  2023/02/23 21:06

TORONTO, ON / ACCESSWIRE / February 23, 2023 / Eskay Mining Corp. ("Eskay" or the "Company") (TSXV:ESK) (OTCQX:ESKYF) (Frankfurt:KN7)(WKN:A0YDPM) is pleased to announce further encouraging diamond drill results from its 2022 exploration program at its 100% controlled Consolidated Eskay Property in the Golden Triangle, British Columbia.

多倫多,on/ACCESSWIRE/2023年2月23日/Eskay礦業公司(“Eskay”或“公司”)(多倫多證券交易所股票代碼:ESKYF)(法蘭克福股票代碼:KN7)(WKN:A0YDPM)我們很高興地宣佈,在不列顛哥倫比亞省金三角其100%控股的聯合Eskay地產的2022年勘探計劃中,鑽石鑽探取得了進一步令人鼓舞的結果。

"Results from our 2022 exploration season demonstrate Eskay's team has made considerable progress toward unraveling the district-scale potential of VMS mineralization surrounding the Eskay Creek deposit," commented Dr. John DeDecker, VP of Exploration for Eskay Mining Corp. "Achievements of the 2022 exploration program include defining a new trend of VMS mineralization along the Scarlet-Tarn corridor parallel to and approximately seven kilometers east of the Eskay anticline. Tarn Lake and Scarlet Knob are situated along an east-west trending VMS feeder structure hosted by Eskay rhyolite like that seen in the footwall of the Eskay Creek deposit. Mapping and prospecting define a westward stratigraphic younging direction suggesting that stockwork and replacement-style mineralization at Tarn Lake may represent feeders to seafloor-hosted mineralization up-section towards the important Contact Mudstone horizon, host to high-grade mineralization at Eskay Creek. This recognition is a significant step towards meeting our goal of discovering new Eskay Creek-like high-grade VMS systems. Drilling at TV now shows that Au- and Ag-bearing massive sulfide extends 100 m along strike and overlies an even more extensive zone of stockwork mineralization. We are eager to follow up on all of these encouraging results in 2023."

Eskay礦業公司勘探副總裁John DeDecker博士評論説:“2022年勘探季的結果表明,Eskay的團隊在揭開Eskay Creek礦牀周圍VMS礦化的地區規模潛力方面取得了相當大的進展。2022年勘探計劃的成果包括沿着與Eskay背斜平行且以東約7公里的Scarlet-Tarn走廊確定了VMS礦化的新趨勢。塔恩湖和Scarlet Knob位於Eskay流紋巖賦存的東西走向的VMS支流結構上,與Eskay Creek礦牀的下盤相似。測繪和勘探確定了向西的地層年輕方向,表明塔恩湖的網狀和交替式礦化可能代表着向重要的接觸泥巖層上游的海底礦化的饋送,Eskay Creek的高品位礦化賦存於泥巖層。這一認可是朝着實現我們發現新的Eskay Creek式高級VMS系統的目標邁出的重要一步。TV現在的鑽探顯示,含Au和Ag的塊狀硫化物沿走向延伸100米,並覆蓋着更廣泛的網狀礦化帶。我們渴望在2023年跟進所有這些令人鼓舞的結果。

TV Extensional Drilling

電視伸展鑽探

Highlight results:

突出顯示結果:

  • 4.61 gpt Au and 22.17 gpt Ag (4.89 gpt Au Eq) over 6.28m within 2.84 gpt Au and 22.17 gpt Ag (3.13 gpt Au Eq) over 16.36m in hole TV22-105
  • 2.66 gpt Au and 30.45 gpt Ag (3.05 gpt Au Eq) over 10.56m within 1.51 gpt Au and 25.39 gpt Ag (1.83 gpt Au Eq) over 43.09m in hole TV22-120
  • 3.36 gpt Au and 109.50 gpt Ag (4.76 gpt Au Eq) over 2.00m within 1.14 gpt Au and 30.40 gpt Ag (1.53 gpt Au Eq) over 30.56m in hole TV22-97
  • 6.88 gpt Au and 21.00 gpt Ag (7.15 gpt Au Eq) over 1.10m within 1.28 gpt Au and 87.92 gpt Ag (2.41 gpt Au Eq) over 14.95m in hole TV22-109
  • 4.61 gpt Au和22.17 gpt Ag(4.89 gpt Au Eq)在2.84 gpt Au內超過6.28米,在TV22-105孔中超過16.36米以上22.17 gpt Ag(3.13 gpt Au Eq)
  • 2.66 gpt Au和30.45 gpt Ag(3.05 gpt Au Eq)在1.51 gpt Au內超過10.56米,在TV22-120孔中超過43.09米以上25.39 gpt Ag(1.83 gpt Au Eq)
  • 3.36gpt Au和109.50 gpt Ag(4.76gpt Au Eq)在1.14gpt Au內超過2.00米,在TV22-97孔超過30.56米以上
  • 6.88 gpt Au和21.00 gpt Ag(7.15 gpt Au Eq)在1.28 gpt Au內超過1.10米,在TV22-109孔中超過14.95米以上87.92 gpt Ag(2.41 gpt Au Eq)

Drilling at TV in 2022 expanded the footprint of both the Upper Massive Sulfide Zone and Stockwork Zone at TV (Figures 1, 2 and 3). Massive sulfide mineralization now extends approximately 100 m along strike, ranges from 5 to 10 m in thickness, and is characterized by sulfide lenses hosted by intensely silicified carbonaceous mudstone associated with peperitic dacite (Figures 4 and 5). Massive and semi-massive sulfide mineralization overlies an extensive stockwork feeder zone hosted by dacitic and andesitic breccia and peperite. Stockwork mineralization now extends approximately 175 m along strike, 175 m down dip, and ranges in thickness from 50 to 100 m. Significantly, drill holes testing the up-dip extent of the stockwork zone (TV22-106, 108, and 112) intercepted strongly anomalous Au and Ag values with interspersed values over 1 gpt Au equivalent. Rock chip samples collected from the vicinity of these drill holes suggest that this up-dip zone may contain higher grade pockets of Au and Ag mineralization (Figure 2).

2022年在TV的鑽探擴大了TV的上塊狀硫化物帶和斯托克沃克帶的足跡(圖1、2和3)。塊狀硫化物礦化現在沿走向延伸約100米,厚度從5米到10米不等,其特徵是硫化物透鏡由與珍珠質英安巖共生的強烈硅化碳質泥巖賦存(圖4和5)。塊狀和半塊狀硫化物礦化覆蓋在由英安質和安山質角礫巖和珍珠巖賦存的廣泛的網狀供礦帶上。現在,網狀礦化沿走向延伸約175米,向下延伸175米,厚度從50米到100米不等。值得注意的是,測試網狀地帶(TV22-106、108和112)上傾範圍的鑽孔截獲了強烈異常的Au和Ag值,其散佈值超過1 gpt Au當量。從這些鑽孔附近採集的巖屑樣本表明,這一上傾帶可能含有品位較高的金銀礦化(圖2)。

Significant mineralized intervals from 2022 drill holes completed in the vicinity of the TV deposit are presented in the table below. A complete list of the coordinates of drill holes including holes without significant mineralized intercepts is found at the bottom of this release.

下表載列於TV礦牀附近完成的2022個鑽孔以來的重大礦化間隔。在本新聞稿的底部可以找到一個完整的鑽孔座標列表,其中包括沒有重大礦化截獲的鑽孔。

Hole

From (m)

To (m)

Length (m)

Au (gpt)

Ag (gpt)

Au Eq (gpt)

Ag Eq (gpt)

TV22-88

133.30

135.00

1.70

1.22

1.22

1.24

96.38

TV22-97

95.44

126.00

30.56

1.14

30.40

1.53

119.68

includes

114.00

116.00

2.00

3.36

109.50

4.76

371.58

TV22-99

88.72

93.60

4.88

0.70

23.50

1.00

78.17

97.64

103.34

5.70

1.77

19.46

2.02

157.82

includes

102.55

103.34

0.79

8.85

23.00

9.14

713.30

TV22-105

86.72

103.08

16.36

2.84

22.17

3.13

243.78

includes

86.72

93.00

6.28

4.61

22.17

4.89

381.59

and

96.00

101.00

5.00

2.39

25.40

2.71

211.66

TV22-106

2.56

4.60

2.04

1.69

2.38

1.72

134.20

24.91

26.91

2.00

0.78

17.50

1.00

78.30

TV22-108

4.20

6.99

2.79

1.94

6.00

2.02

157.32

15.00

18.00

3.00

1.33

2.17

1.36

105.76

TV22-109

50.05

65.00

14.95

1.28

87.92

2.41

188.00

includes

50.05

51.15

1.10

6.88

21.00

7.15

557.64

and

57.58

63.23

5.65

1.03

173.12

3.25

253.38

TV22-110

72.27

88.95

16.68

1.44

19.62

1.69

131.55

TV22-111

51.56

58.78

7.22

0.45

92.99

1.64

127.96

includes

54.83

56.51

1.68

0.87

309.00

4.84

377.21

TV22-112

0.00

7.00

7.00

0.75

9.31

0.87

68.05

includes

4.00

5.00

1.00

3.57

8.18

3.67

286.64

TV22-120

127.79

170.88

43.09

1.51

25.39

1.83

142.83

includes

130.18

131.00

0.82

4.19

15.00

4.38

341.82

and

136.58

147.14

10.56

2.66

30.45

3.05

238.18

TV22-121

95.00

97.18

2.18

0.13

121.87

1.69

131.82

128.31

132.00

3.69

1.27

40.31

1.79

139.37

孔洞

發件人(M)

至(M)

長度(米)

Au(GPT)

AG(GPT)

Au Eq(GPT)

AG EQ(GPT)

TV22-88

133.30

135.00

1.70

1.22

1.22

1.24

96.38

TV22-97

95.44

126.00

30.56

1.14

30.40

1.53

119.68

包括

114.00

116.00

2.00

3.36

109.50

4.76

371.58

電視22-99

88.72

93.60

4.88

0.70

23.50

1.00

78.17

97.64

103.34

5.70

1.77

19.46

2.02

157.82

包括

102.55

103.34

0.79

8.85

23.00

9.14

713.30

TV22-105

86.72

103.08

16.36

2.84

22.17

3.13

243.78

包括

86.72

93.00

6.28

4.61

22.17

4.89

381.59

96.00

101.00

5.00

2.39

25.40

2.71

211.66

TV22-106

2.56

4.60

2.04

1.69

2.38

1.72

134.20

24.91

26.91

2.00

0.78

17.50

1.00

78.30

TV22-108

4.20

6.99

2.79

1.94

6.00

2.02

157.32

15.00

18.00

3.00

1.33

2.17

1.36

105.76

TV22-109

50.05

65.00

14.95

1.28

87.92

2.41

188.00

包括

50.05

51.15

1.10

6.88

21.00

7.15

557.64

57.58

63.23

5.65

1.03

173.12

3.25

253.38

TV22-110

72.27

88.95

16.68

1.44

19.62

1.69

131.55

TV22-111

51.56

58.78

7.22

0.45

92.99

1.64

127.96

包括

54.83

56.51

1.68

0.87

309.00

4.84

377.21

TV22-112

0.00

7.00

7.00

0.75

9.31

0.87

68.05

包括

4.00

5.00

1.00

3.57

8.18

3.67

286.64

TV22-120

127.79

170.88

43.09

1.51

25.39

1.83

142.83

包括

130.18

131.00

0.82

4.19

15.00

4.38

341.82

136.58

147.14

10.56

2.66

30.45

3.05

238.18

TV22-121

95.00

97.18

2.18

0.13

121.87

1.69

131.82

128.31

132.00

3.69

1.27

40.31

1.79

139.37

Au Eq and Ag Eq values have all been adjusted to the silver-to-gold ratio of 78:1 for this news release.

在本新聞稿中,Au Eq和Ag Eq的值都已調整為78:1的白銀與黃金的比例。

Tarn Lake

塔恩湖

Assay results from the maiden drill program at Tarn Lake have already defined an 80m-long open-ended trend of Au mineralization that dips west-northwest (Figures. 1, 7 and 8). Rock chip sample results suggest that Au mineralization extends up-dip from the drill holes to the surface. Mineralization remains open down-dip.

塔恩湖首次鑽探項目的化驗結果已經確定了一個80米長的無限制的金礦化趨勢,該趨勢向西北偏西傾斜(圖1)。1、7和8)。巖屑樣品結果表明,金礦化從鑽孔向上延伸到地表。礦化仍然是敞開的向下傾角。

Sulfide mineralization intercepted by drilling is dominantly replacement-style and stockwork-style (Figure 9), and is hosted by intensely altered Eskay rhyolite. This style of mineralization and intense hydrothermal alteration are consistent with a position in the immediate sub-seafloor environment of a VMS feeder zone. Geological mapping, drilling, and lithological facies analyses show extensive rhyolite-bearing volcaniclastic debris flow beds, peperitic rhyolite, and flow-banded rhyolite defining a rhyolite dome complex that formed at a paleoseafloor position proximal to a syn-volcanic VMS feeder structure, supporting the interpretation based on mineralization and alteration. Based on this geology, Eskay's exploration team thinks there is considerable potential for the presence of seafloor-hosted VMS mineralization at one or more horizons at Tarn Lake, as is seen along the parallel Eskay Creek-Sib-Lulu trend to the west (Figure 10).

鑽探截獲的硫化物礦化以交替型和網狀型為主(圖9),賦存於強烈蝕變的Eskay流紋巖中。這種類型的礦化和強烈的熱液蝕變與VMS饋送帶的緊鄰海底下環境中的位置一致。地質填圖、鑽探和巖相分析表明,廣泛的含流紋巖火山碎屑泥石層、珍珠巖流紋巖和流帶流紋巖定義了流紋巖穹隆雜巖,形成於同火山VMS饋送構造附近的古海底位置,支持基於礦化和蝕變的解釋。基於這種地質情況,Eskay的勘探團隊認為,在塔恩湖的一個或多個層位存在海底託管的VMS礦化的潛力很大,正如西邊平行的Eskay Creek-Sib-Lulu趨勢所看到的那樣(圖10)。

Eskay's geological mapping team has determined that the stratigraphic younging direction along the Scarlet-Tarn trend is to the west, and that the contact between the Eskay rhyolite and the Willow Ridge basalt lies to the west of Tarn Lake (Figure 10). The contact between these lithologies defines the Contact mudstone horizon that hosts the world-class Au-Ag mineralization at Eskay Creek Mine. Given that recent rock chip sampling indicates Au mineralization continues west of Tarn Lake, it is possible the Tarn VMS system continues up-stratigraphy to the Contact mudstone horizon. These findings are a significant step towards our goal of finding Eskay Creek-like VMS deposits on the Consolidated Eskay Property.

Eskay的地質填圖團隊已經確定,沿着Scarlet-Tarn趨勢的地層年輕方向是向西的,Eskay流紋巖和柳嶺玄武巖的接觸位於Tarn湖以西(圖10)。這些巖性之間的接觸定義了Eskay Creek礦世界級Au-Ag礦化所在的接觸泥巖層。考慮到最近的巖屑採樣表明,塔恩湖以西的金礦化仍在繼續,塔恩VMS系統可能會沿着地層向上延伸到接觸泥巖層。這些發現是朝着我們在Eskay綜合地產上找到Eskay Creek式VMS礦藏的目標邁出的重要一步。

In addition to the potential for Au and Ag mineralization down-dip and up-section from 2022 drilling, there is considerable potential for mineralization to extend beneath Bruce Glacier to Scarlet Knob along east-west trending feeder structures (Figure 11). These feeder structures are delineated by andesite dikes surrounded by sulfide mineralization and intense hydrothermal alteration of the host Eskay rhyolite.

自2022年鑽探以來,金銀礦化的潛力除了向下傾斜和向上延伸外,還有相當大的潛力沿着東西走向的支流構造在布魯斯冰川下方延伸至Scarlet Knob(圖11)。安山巖脈巖被硫化物礦化和寄主Eskay流紋巖強烈的熱液蝕變包圍,圈定了這些饋源構造。

Significant drill results from hole TN22-8 completed at Tarn Lake are presented in the table below.

在塔恩湖完成的TN22-8孔的重要鑽探結果見下表。

Hole

From (m)

To (m)

Length (m)

Au (gpt)

Ag (gpt)

Au Eq (gpt)

Ag Eq (gpt)

TN22-8

90.19

92.88

2.69

0.75

29.00

1.12

87.50

117.33

123.00

5.67

1.37

3.37

1.41

110.00

133.53

139.72

6.19

1.46

2.13

1.49

116.16

158.04

161.00

2.96

1.27

4.11

1.32

102.78

孔洞

發件人(M)

至(M)

長度(米)

Au(GPT)

AG(GPT)

Au Eq(GPT)

AG EQ(GPT)

TN22-8

90.19

92.88

2.69

0.75

29.00

1.12

87.50

117.33

123.00

5.67

1.37

3.37

1.41

110.00

133.53

139.72

6.19

1.46

2.13

1.49

116.16

158.04

161.00

2.96

1.27

4.11

1.32

102.78

Au Eq and Ag Eq values have all been adjusted to the silver-to-gold ratio of 78:1 for this news release.

在本新聞稿中,Au Eq和Ag Eq的值都已調整為78:1的白銀與黃金的比例。

2022 Exploration Program

2022年探索計劃

The fundamental goal of the 2022 exploration program was to identify new precious metal-rich VMS deposits across the Consolidated Eskay Project through early-stage work including mapping and geochemical sampling, and more advanced work including widely spaced drilling. During the 2022 exploration season, Eskay Mining successfully completed 29,500m of diamond drilling along the TV-Jeff corridor and along the Scarlet Ridge-Tarn Lake trend.

2022年勘探計劃的基本目標是通過包括測繪和地球化學採樣在內的早期工作以及包括大範圍鑽探在內的更高級工作,在聯合Eskay項目中發現新的富含貴金屬的VMS礦牀。2022年勘探季期間,艾斯凱礦業在TV-Jeff走廊和紅嶺-塔恩湖潮流沿線成功完成了29,500米的鑽石鑽探。

Drill results discussed in this news release come from holes drilled in the vicinity of the TV deposit and the newly discovered Tarn Lake mineralizing system. As of this news release, all assays have returned from the 2022 drill program.

本新聞稿中討論的鑽探結果來自TV礦牀附近的鑽孔和新發現的Tarn Lake成礦系統。截至本新聞稿,2022年演習計劃的所有化驗結果都已返回。

Au Eq and Ag Eq Calculations and True Width:

Au Eq和Ag Eq計算和實際寬度:

Note on use of Au eq (Au eq=Au+Ag/78) and Ag eq (Ag eq=Au*78+Ag): Mineralization at the TV and Jeff deposits displays similar characteristics and mineralogy to the Eskay Creek deposit and therefore for Au eq, and Au:Ag, a ratio of 78:1 is used and Au eq and Ag eq values are deemed to be reasonable based on assumed gold recovery (84.2%) and silver recovery (87.3%) as reported in the Eskay Creek Project NI 43-101 Technical Report and Prefeasibility Study, British Columbia, Canada, Effective Date: 22 July, 2021, Prepared for: Skeena Resources Ltd., Prepared by: Absence Engineering Canada Inc.

關於Au eq(Au eq=Au+Ag/78)和Ag eq(Ag eq=Au*78+Ag)的使用説明:TV和Jeff礦牀的礦化顯示出與Eskay Creek礦牀相似的特徵和礦物學,因此對於Au eq和Au:Ag,採用78:1的比例,並根據假設的金回收率(84.2%)和銀回收率(87.3%)被認為是合理的,如加拿大不列顛哥倫比亞省Eskay Creek項目NI 43-101技術報告和預可行性研究,有效日期:2021年7月22日,為:Skeena Resources Ltd編制。編寫人:加拿大缺勤工程公司。

True widths of reported intercepts are not fully understood at this time but given the moderately dipping tabular nature of these deposits and the steep angle of drilling, Eskay geologists estimate true widths represent approximately 70-90% of the reported drill intercept lengths.

目前還不能完全瞭解報告的截距的真實寬度,但考慮到這些礦牀的中等傾角板狀性質和鑽井的陡峭角度,Eskay地質學家估計,真實寬度約佔報告的鑽井截距長度的70%-90%。

QA/QC, Methodology Statement:

QA/QC,方法聲明:

Halved HQ drill core samples are submitted to ALS Geochemistry in Terrace, British Columbia for preparation and analysis. ALS is accredited to the ISO/IEC 17025 standard for gold assays. All analytical methods include quality control standards inserted at set frequencies. The entire sample interval is crushed and homogenized, 250 g of the homogenized sample is pulped. All samples were analyzed for gold, silver, mercury, and a suite of 48 major and trace elements. Analysis for gold is by fire assay fusion followed by Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES) on 30 g of pulp. Analysis for silver is by fire assay and gravimetric analysis on 30 g of pulp. Mercury is analyzed using the trace Hg Inductively Coupled Plasma Mass Spectroscopy (ICP-MS) method. All other major and trace elements are analyzed by four-acid digestion followed by ICP-MS.

減半的HQ鑽芯樣本被提交給不列顛哥倫比亞省Terrace的ALS地球化學公司進行準備和分析。肌萎縮側索硬化症已通過國際標準化組織/國際電工委員會17025黃金檢測標準。所有分析方法都包括按設定頻率插入的質量控制標準。整個樣品間隔被粉碎和均質,250克均化的樣品被製漿。對所有樣品進行了金、銀、汞以及48種常量和微量元素的分析。金的分析採用火試金,然後對30克紙漿進行電感耦合等離子體原子發射光譜(ICPAES)分析。銀的分析是用火試法和30克紙漿的重量分析。用痕量汞的電感耦合等離子體質譜(ICP-MS)方法分析汞。採用四酸消化-電感耦合等離子體質譜(ICP-MS)對所有其他常量和微量元素進行分析。

Historical rock chip sample data is sourced from Assessment Report AR19675 by Granges dated February 7, 1990. Eskay Mining is unable to fully verify this data, and it should be treated as such by the reader.

歷史巖屑樣本數據來源於Grange於1990年2月7日發佈的評估報告AR19675。Eskay Mining無法完全核實此數據,讀者應將其視為此類數據。

Dr. Quinton Hennigh, P. Geo., a Director of the Company and its technical adviser, a qualified person as defined by National Instrument 43-101, has reviewed and approved the technical contents of this news release.

公司董事及其技術顧問Quinton Hennigh博士已審核並批准了本新聞稿的技術內容。Quinton Hennigh博士是National Instrument 43-101定義的合格人員。

About Eskay Mining Corp:

關於Eskay礦業公司:

Eskay Mining Corp (TSX-V:ESK) is a TSX Venture Exchange listed company, headquartered in Toronto, Ontario. Eskay is an exploration company focused on the exploration and development of precious and base metals along the Eskay rift in a highly prolific region of northwest British Columbia known as the "Golden Triangle," 70km northwest of Stewart, BC. The Company currently holds mineral tenures in this area comprised of 177 claims (52,600 hectares).

Eskay礦業公司(多倫多證券交易所股票代碼:ESK)是一家在多倫多證券交易所上市的公司,總部設在安大略省多倫多。Eskay是一家勘探公司,專注於沿着不列顛哥倫比亞省西北部Eskay裂谷勘探和開發貴金屬和賤金屬。Eskay裂谷位於不列顛哥倫比亞省西北部,位於不列顛哥倫比亞省斯圖爾特西北70公里處,被稱為“金三角”。本公司目前持有該地區的礦產所有權,包括177項權利主張(52,600公頃)。

All material information on the Company may be found on its website at and on SEDAR at .

有關公司的所有重要信息均可在公司網站和SEDAR網站上找到。

For further information, please contact:

如需更多信息,請聯繫:

Mac Balkam T: 416 907 4020
President & Chief Executive Officer E: Mac@eskaymining.com
Mac Balkam T: 416 907 4020
總裁&首席執行官 郵箱:mac@eskaymining.com

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.

都不是多倫多證券交易所及其監管服務提供商(該術語在多倫多證券交易所的政策中定義)對本新聞稿的充分性或準確性承擔責任。

Forward-Looking Statements: This Press Release contains forward-looking statements that involve risks and uncertainties, which may cause actual results to differ materially from the statements made. When used in this document, the words "may", "would", "could", "will", "intend", "plan", "anticipate", "believe", "estimate", "expect" and similar expressions are intended to identify forward-looking statements. Such statements reflect our current views with respect to future events and are subject to risks and uncertainties. Many factors could cause our actual results to differ materially from the statements made, including those factors discussed in filings made by us with the Canadian securities regulatory authorities. Should one or more of these risks and uncertainties, such as actual results of current exploration programs, the general risks associated with the mining industry, the price of gold and other metals, currency and interest rate fluctuations, increased competition and general economic and market factors, occur or should assumptions underlying the forward looking statements prove incorrect, actual results may vary materially from those described herein as intended, planned, anticipated, or expected. We do not intend and do not assume any obligation to update these forward-looking statements, except as required by law. Shareholders are cautioned not to put undue reliance on such forward-looking statements.

轉發-外觀聲明:本新聞稿包含涉及風險和不確定因素的前瞻性陳述,可能會導致實際結果與所作陳述大相徑庭。在本文件中使用的“可能”、“將”、“可能”、“將”、“打算”、“計劃”、“預期”、“相信”、“估計”、“預期”等詞語以及類似的表述都是為了識別前瞻性陳述。這些陳述反映了我們目前對未來事件的看法,受到風險和不確定因素的影響。許多因素可能會導致我們的實際結果與聲明大不相同,包括我們向加拿大證券監管機構提交的文件中討論的那些因素。如果這些風險和不確定性中的一個或多個發生,例如當前勘探計劃的實際結果、與採礦業相關的一般風險、黃金和其他金屬的價格、貨幣和利率波動、競爭加劇以及一般經濟和市場因素,或者前瞻性陳述所依據的假設被證明是不正確的,實際結果可能與本文中描述的預期、計劃、預期或預期的結果大不相同。我們不打算也不承擔任何義務更新這些前瞻性陳述,除非法律要求。告誡股東不要過度依賴此類前瞻性陳述。.

Table of locations and orientations of drill holes reported in this release

本新聞稿中報告的鑽孔位置和方向表

Hole ID

Easting (m)

Northing (m)

Elevation (m)

Azimuth

Dip

Total Depth (m)

J22-123

410077

6267479

530

270

52

485

J22-124

410051

6267243

543

270

55

489

J22-125

409816

6268745

416

250

50

264

TV22-88

409501

6266788

439

282

45

384

TV22-91

409675

6266449

621

282

45

469

TV22-92

409627

6266109

695

282

45

201

TV22-93

409686

6266197

711

282

45

349

TV22-94

409675

6266449

621

102

78

103

TV22-95

409590

6265980

727

282

55

406

TV22-96

409590

6265980

727

-

90

172

TV22-97

409590

6265980

727

217

45

234

TV22-98

409343

6265980

678

282

70

328

TV22-99

409590

6265980

727

190

45

186

TV22-100

409619

6266027

712

282

60

250

TV22-101

409343

6265980

678

-

90

161

TV22-102

409619

6266027

712

210

45

75

TV22-103

409590

6265929

750

300

75

150

TV22-105

409590

6265851

792

300

80

150

TV22-106

409354

6265847

736

282

70

103

TV22-108

409459

6265841

773

282

60

444

TV22-109

409590

6265851

792

240

55

189

TV22-110

409590

6265851

792

240

75

253

TV22-111

409590

6265851

792

215

55

202

TV22-112

409459

6265841

773

-

90

121

TV22-113

409590

6265851

792

215

75

250

TV22-114

409324

6265755

762

282

45

135

TV22-115

409590

6265851

792

180

55

239

TV22-116

409541

6265719

844

282

55

212

TV22-117

409590

6265851

792

90

70

230

TV22-118

409902

6265721

987

290

49

525

TV22-119

409585

6265763

820

10

55

275

TV22-120

409585

6265763

820

350

55

308

TV22-121

409585

6265763

820

340

65

182

TV22-122

409585

6265763

820

-

90

203

TV22-123

409585

6265763

820

200

45

202

TN22-04

415102

6273575

1470

100

55

123

TN22-05

415165

6273652

1444

87

55

113

TN22-07

415165

6273652

1444

50

55

155

TN22-08

415102

6273575

1470

125

70

163

TN22-09

415165

6273652

1444

80

70

208

TN22-11

415165

6273652

1444

-

90

127

孔ID

東距(M)

北距(M)

高程(米)

方位角

浸漬

總深度(米)

J22-123

410077

6267479

530

270

52

485

J22-124

410051

6267243

543

270

55

489

J22-125

409816

6268745

416

250

50

264

TV22-88

409501

6266788

439

282

45

384

TV22-91

409675

6266449

621

282

45

469

TV22-92

409627

6266109

695

282

45

201

TV22-93

409686

6266197

711

282

45

349

TV22-94

409675

6266449

621

102

78

103

電視22-95

409590

6265980

727

282

55

406

電視22-96

409590

6265980

727

-

90

172

TV22-97

409590

6265980

727

217

45

234

TV22-98

409343

6265980

678

282

70

328

電視22-99

409590

6265980

727

190

45

186

TV22-100

409619

6266027

712

282

60

250

TV22-101

409343

6265980

678

-

90

161

TV22-102

409619

6266027

712

210

45

75

TV22-103

409590

6265929

750

300

75

150

TV22-105

409590

6265851

792

300

80

150

TV22-106

409354

6265847

736

282

70

103

TV22-108

409459

6265841

773

282

60

444

TV22-109

409590

6265851

792

240

55

189

TV22-110

409590

6265851

792

240

75

253

TV22-111

409590

6265851

792

215

55

202

TV22-112

409459

6265841

773

-

90

121

TV22-113

409590

6265851

792

215

75

250

TV22-114

409324

6265755

762

282

45

135

TV22-115

409590

6265851

792

180

55

239

TV22-116

409541

6265719

844

282

55

212

TV22-117

409590

6265851

792

90

70

230

TV22-118

409902

6265721

987

290

49

525

TV22-119

409585

6265763

820

10

55

275

TV22-120

409585

6265763

820

350

55

308

TV22-121

409585

6265763

820

340

65

182

TV22-122

409585

6265763

820

-

90

203

TV22-123

409585

6265763

820

200

45

202

TN22-04

415102

6273575

1470

100

55

123

TN22-05

415165

6273652

1444

87

55

113

TN22-07

415165

6273652

1444

50

55

155

TN22-08

415102

6273575

1470

125

70

163

TN22-09

415165

6273652

1444

80

70

208

TN22-11

415165

6273652

1444

-

90

127

(Figure 1: Geologic map showing a new interpretation for the distribution of mineralized stratigraphy of the Eskay Creek area with gold in surface samples. Map displays correlative domains where upper Hazelton Group Eskay rhyolite is host to VMS mineralization along the Scarlet-Tarn trend. Also labeled are VMS showings along extensions of the Eskay Anticline to the south at SIB-Lulu, Hexagon-Mercury, TV-Jeff, and Excelsior.)
(圖1:地質圖顯示了對Eskay Creek地區礦化地層分佈的新解釋,地表樣品中有金。MAP顯示了沿Scarlet-Tarn走向上黑茲爾頓羣Eskay流紋巖是VMS成礦的容礦區域。同時標記的還有沿艾斯凱背斜向南延伸的SIB-Lulu、六角形-水星、TV-Jeff和Excelsior的VMS顯示。)
(Figure 2: Map showing locations of 2022 drill collars and traces, and Au assay results for recent and legacy rock chip samples at TV. Mineralization is concentrated in the zone marked by the ellipse, and extends from the surface down-dip ~150 m. The cluster of high-grade samples near TV22-106 and TV22-108 suggest this extension of the stockwork zone may contain higher grade pockets of Au and Ag mineralization.)
(圖2:在電視上顯示2022個鑽環和痕跡的位置的地圖,以及最近和遺留巖屑樣本的金分析結果。礦化集中在以橢圓形為標誌的帶中,從地表向下延伸約150m。TV22-106和TV22-108附近的高品位樣品簇表明,該網狀帶的延伸可能含有較高品位的金銀礦化帶。
(Figure 3: Map and cross-section views of TV showing drill hole and rock chip assay results. Cross-sections are shown in the continuation of this figure below, and are 100 m thick along east-west lines spaced 50 meters apart. Assay results for 2022 drill holes are shown in bold, with results from 2020-2021 drilling shown as fine lines. Drilling in 2022 expanded the footprint of the Upper Massive Sulfide Zone northwards and down-dip with respect to 2020-2021 drilling, giving this zone minimum dimensions of ~100 m along strike, ~150 m down-dip to the east, and a true thickness of ~ 5-10 m. The footprint of the Stockwork Zone was expanded down-dip to the east, and up-dip to the west with respect to 2020-2021 drill holes, giving this zone dimensions of ~175 m along strike, 170 m down-dip, and a true thickness ranging from ~50-100 m. Recent and legacy rock chip sample results suggest that the up-dip part of the Stockwork Zone may contain high-grade pockets of Au and Ag mineralization within a zone of strongly anomalous Au and Ag mineralization.)
(圖3:顯示鑽孔和巖屑分析結果的電視地圖和橫斷面圖。橫截面如下圖所示,沿東西相距50米的線厚100米。2022個鑽孔的化驗結果以粗體顯示,2020-2021年鑽探的結果以細線顯示。2022年的鑽井擴大了上塊狀硫化物帶的足跡,相對於2020-2021年的鑽井,該帶的足跡向北擴展和向下傾斜,使該帶沿走向的最小尺寸為~100米,向東的下傾角為~150米,真厚度為~5-10米。對2020-2021年的鑽孔,斯圖克區的足跡向東擴大,向西向上傾斜,使該帶的走向尺寸為~175米,向下傾斜170米,新的和遺留的巖屑樣品結果表明,斯托克沃克帶的上傾部分可能在金銀礦化強烈異常的帶內含有高品位的金銀礦化帶。
(Figure 3 continued.)
(圖3繼續。)
(Figure 3 continued.)
(圖3繼續。)
(Figure 4: Representative intercept of massive sulfide from TV22-109 50.47-62.72 m, showing the association of sulfide mineralization with intensely silicified mudstone and peperitic dacite.)
(圖4:TV22-10950.47-62.72m塊狀硫化物的代表性截距,顯示硫化物礦化與強烈硅化泥巖和榴輝巖英安巖共生。)
(Figure 5: TV22-105 87.41-97.27 m showing semi-massive and stockwork sulfide mineralization hosted by intensely silicified mudstone, with overlying dacite breccia.)
(圖5:TV22-105 87.41-97.27米顯示半塊狀和網狀硫化物礦化,賦存於強烈硅化泥巖中,上覆英安巖角礫巖。)
(Figure 6: TV22-120 133.81-146.20 m showing stockwork sulfide mineralization hosted by intensely silicified mudstone. This style mineralization is identical to that intercepted by drill holes TV21-63, TV21-66, and TV21-67, with the later hole ranging from 25-40 m up-dip from TV22-120. TV22-120 was drilled sub-parallel to strike and does not represent true thickness.)
(圖6:TV22-120 133.81-146.20米顯示強烈硅化泥巖賦存的網狀硫化物礦化。這種類型的礦化與TV21-63、TV21-66和TV21-67鑽孔截獲的礦化相同,後者的鑽孔從TV22-120向上傾斜25-40m。TV22-120是次平行於走向鑽進的,並不代表真實厚度。)
(Figure 7: Map of Tarn Lake showing drone imagery, 2022 drill traces with Au-bearing intercepts highlighted in blue, and Assay results with locations for legacy and 2022 rock chip samples.)
(圖7:塔恩湖地圖,顯示無人機圖像,2022年鑽探痕跡,以藍色突出顯示含金截獲,以及Assay結果,顯示遺留和2022年巖屑樣本的位置。)
(Figure 8: Assay results from the maiden drill program and rock chip sampling at Tarn Lake. The top figure is a map view showing the location of the 200 m thick cross-section C-C' at bottom. Drill holes TN22-10, TN22-12, TN22-8, and TN22-6 define an 85 m long trend of Au mineralization along strike. Drilling combined with rock chip sampling indicate a west-northwest dipping zone of mineralization extending from the surface ~75 m down-dip. Mineralization is open down-dip. Eskay's mapping team has determined that the stratigraphic younging direction is to the west. This, combined with the Au-bearing rock chip samples to the west indicate VMS mineralization continues up-stratigraphy.)
(圖8:塔恩湖的首次鑽探計劃和巖屑取樣的化驗結果。上圖是地圖視圖,顯示了底部200米厚的橫截面C-C‘的位置。鑽孔Tn22-10、Tn22-12、Tn22-8和Tn22-6定義了沿走向的85米長的金礦化趨勢。鑽探結合巖屑取樣表明,礦化呈西北向傾斜帶,從地表向下延伸約75m。礦化呈開闊下傾。Eskay的測繪團隊已經確定地層的年輕方向是向西。這與西側含金巖屑樣品相結合,表明VMS成礦作用繼續向上地層。)
(Figure 9. TN22-8 133.33-141.36 showing representative stockwork mineralization hosted by Eskay rhyolite. The interval shown contains the 6.19 m intercept grading 1.49 g/t Au equivalent, and shows that rock with relatively low sulfide abundance contains appreciable gold, suggesting strong enrichment of gold with respect to sulfide minerals.)
(圖9.Tn22-8 133.33-141.36顯示以埃斯凱流紋巖為容礦的典型網狀礦化。顯示的間隔包含6.19m截距分級1.49g/t Au當量,並表明硫化物丰度相對較低的巖石含有可觀的金,表明金相對於硫化物礦物具有強烈的富集性。)
(Figure 10: Geological map showing the Eskay anticline and Scarlet-Tarn trends of VMS mineralization. Geological mapping of the Scarlet-Tarn trend by Eskay's team in 2022 has determined that the stratigraphic younging direction is to the west, and that the Eskay rhyolite host to mineralization at Tarn Lake is overlain by Willow Ridge basalt to the west. The contact between these two lithologies define the Contact mudstone horizon, the host to the world-class mineralization at Eskay Creek mine. This finding is a significant step towards our goal of finding Eskay Creek-like VMS deposits.)
(圖10:顯示VMS礦化的Eskay背斜和Scarlet-Tarn趨勢的地質圖。Eskay的團隊在2022年對Scarlet-Tarn趨勢進行的地質填圖確定了地層的年輕方向是向西的,塔恩湖成礦的Eskay流紋巖在西部被柳嶺玄武巖覆蓋。這兩種巖性之間的接觸定義了接觸泥巖層,這是Eskay Creek礦世界級礦化的宿主。這一發現是朝着我們尋找類似Eskay Creek的VMS礦牀的目標邁出的重要一步。)
(Figure 11: Cross-section view of Tarn Lake and Scarlet Knob looking due south, showing assay results for 2022 drill holes and rock chip samples. Mineralization at both showings is hosted the Eskay rhyolite, and is focused along east-west trending andesite dikes that likely represent the syn-volcanic feeder structures that fed VMS mineralization in the area. Given that mineralization is focused along east-west trending structures, and the high Au and Ag grades from rock chip samples along the margins of Bruce Glacier, it is possible that mineralization extends under Bruce Glacier and connects Tarn Lake and Scarlet Knob.)
(圖11:塔恩湖和Scarlet Knob正南方的橫斷面圖,顯示了2022個鑽孔和巖屑樣本的分析結果。這兩個礦體的礦化賦存於Eskay流紋巖中,並沿東西走向的安山巖脈巖集中,這些安山巖可能代表了為該區VMS成礦提供了同源火山饋送構造。考慮到礦化沿着東西走向的構造集中,以及布魯斯冰川邊緣巖屑樣品中的高Au和Ag品位,礦化有可能延伸到布魯斯冰川之下,連接塔恩湖和Scarlet Knob。)

SOURCE: Eskay Mining Corp.

資料來源:埃斯凱礦業公司


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