Snow Lake Lithium Provides Final Update Following Successful Completion of the 2022 Grass River Drilling Campaign
Snow Lake Lithium Provides Final Update Following Successful Completion of the 2022 Grass River Drilling Campaign
Results:
結果:
-
2.0 % Li2O over 16 meters starting at 30.9 meters down hole (CBP-007)
- Including 3.1 % Li2O over 1.5 meters
-
1.8 % Li2O over 3.0 meters starting at 210.3 meters down hole (GRP-018)
- Including 3.6 % Li2O over 1.5 meters
-
2.0 % Li2O over 6.0 meters starting at 125.0 meters down hole (GRP-013)
- Including 3.2 % Li2O over 1.5 meters
-
2.9 % Li2O over 2.3 meters starting at 84.2 meters down hole (GRP-021)
- Including 3.2 % Li2O over 1.5 meters
- Media Assets can be downloaded here: Snow Lake Lithium - Grass River Drilling Campaign
-
2.0%Li2O從井下30.9米開始,超過16米(CBP-007)
- 包括3.1%的Li2O超過1.5米
-
1.8%Li2O從井下210.3米開始,超過3米(GRP018)
- 包括3.6%的Li2O超過1.5米
-
2.0%Li2O從井下125.0米開始,超過6米(013級)
- 包括3.2%的Li2O超過1.5米
-
2.9%Li2O從井下84.2米開始,超過2.3米(GRP-021)
- 包括3.2%的Li2O超過1.5米
- 媒體資產可在此處下載:雪湖鋰-草河鑽探活動
WINNIPEG, MB / ACCESSWIRE / January 11, 2023 / Snow Lake Resources Ltd., d/b/a Snow Lake Lithium Ltd. (NASDAQ:LITM) ("Snow Lake" or the "Company"), today announced the final drill results and an update and analysis following the recently completed 2022 Grass River drilling campaign. All geochemical analyses from SGS Laboratories Canada Inc. of Lakefield, Ontario ("SGS Lakefield") have been received and significant intersections are listed in Table 1.0 with the new drill results highlighted in black bold text for reference.
温尼伯,MB/ACCESSWIRE/2023年1月11日/雪湖資源有限公司,d/b/a雪湖鋰業有限公司(納斯達克股票代碼:LITM)(以下簡稱“雪湖”或“公司”)今天宣佈了最終鑽探結果,以及繼最近完成的2022年草河鑽探活動之後的最新情況和分析。來自安大略省萊克菲爾德的SGS實驗室加拿大公司(“SGS Lakefield”)的所有地球化學分析都已收到,表1.0列出了重要的交叉點,新的鑽探結果以黑色粗體突出顯示,以供參考。
The pegmatite geology in the Grass River area ("GRP") is significantly more complex than the Thompson Brothers Lithium dyke, which was recognized early in the drill campaign. As noted by several geologists at the core house, several intersections of coarse-grained spodumene pegmatites were logged in multiple holes within the Grass River area. Due to this level of complexity, Snow Lake engaged SGS Lakefield to assist with modeling the GRP dyke to better understand the three-dimensional (3D) composition of the subsurface area.
草河地區的偉晶巖地質明顯比湯普森兄弟鋰堤複雜得多,湯普森兄弟鋰堤在鑽探活動早期就被發現了。正如核心房屋的幾位地質學家所指出的那樣,在草河地區的多個洞中記錄了幾個粗粒鋰輝石偉晶巖的交叉點。由於這種複雜程度,雪湖聘請了SGS Lakefield協助對GRP堤壩進行建模,以更好地瞭解地下區域的三維(3D)組成。
Based on the final wireframe modeling of the pegmatite dykes at Grass River, SGS Lakefield was able to identify a minimum of three distinctive spodumene bearing pegmatite dykes. Snow Lake's technical personnel in the field hypothesized that there could be as many as five distinctive dykes based on core and field observations. Due to this higher density of dykes within the Grass River area, Snow Lake will refer to this area as the "GRP Dykes Swarm" as the Company's drilling campaign progresses.
根據Grass River偉晶巖牆的最終線框模型,SGS Lakefield至少能夠識別出三個不同的含鋰輝石偉晶巖牆。雪湖現場的技術人員根據巖心和現場觀察推測,可能有多達五個不同的堤壩。由於草河地區的堤壩密度較高,隨着公司鑽探活動的進行,雪湖將把該地區稱為“GRP堤壩羣”。
Significant high grade Li2O intercepts continue to be produced by the GRP Dykes Swarm and to infer a compelling lithium presence beyond the resource identified from the initial scoping study. Drill holes GRP-013 and GRP-021 both returned a 1.5-meter intercept of 3.2% Li2O while the highest recorded intercept of 3.6% Li2O was retrieved from hole GRP-018. These intercepts have been recovered from between 80 and 200 meters down hole, which suggests that Li2O levels may be rising at greater depths (See Table 1.0, Figure 1.0 and Sections 2, 3 and 4).
顯着高分Li2O GRP堤壩羣繼續產生截獲,並推斷存在令人信服的鋰存在,超出了最初範圍研究確定的資源範圍。GRP013和GRP021號鑽孔均返回3.2%的1.5米截距Li2O而最高記錄截獲3.6%Li2O是從GRP-018孔中取回的。這些截獲的東西是在80到200米的井下發現的,這表明Li2O水平可能在更深的地方上升(參見表1.0、圖1.0以及第2、3和4節)。
A stunning interval of 16.0 meters of 2.0% Li2O, including a 1.5-meter intercept of 3.1% Li2O, was obtained by drill hole CBP-007. This hole, which was collared on the main deposit's North-West strike extension, shows that the dyke has remarkable continuity (See Section 1). As the Company focuses on expanding its identified resource base within the GRP Dykes Swarm, the North-West extension will be the focus of the winter drilling program in 2023.
令人驚歎的16.0米間隔2.0%Li2O,包括1.5米攔截3.1%Li2O,通過CBP-007鑽孔獲得。這個洞是在主要礦牀的西北走向延伸上套上的,表明堤壩具有顯著的連續性(見第1節)。隨着公司專注於擴大其在GRP堤壩羣內已確定的資源基礎,西北延伸將是2023年冬季鑽探計劃的重點。
Dale Schultz, Snow Lake's Project Manager and VP of Resource Development, commented, "The results of the 2022 Grass River drilling campaign demonstrate the Company's continued success in expanding its identified resource base and evaluating additional pegmatites for lithium extraction. Our analysis, completed in collaboration with SGS Lakefield, has shown that the high-grade lithium intercepts confirm the presence of Li2O deposits in the GRP Dykes Swarm with further investigation required at depth. As we begin the 2023 winter drilling program, we look forward to examining the North-West extension of the GRP area and advancing our resource expansion plans over the coming months."
雪湖項目經理兼資源開發副總裁戴爾·舒爾茨他説:“2022年草河鑽探活動的結果表明,公司在擴大已確定的資源基礎和評估更多用於提鋰的偉晶巖方面繼續取得成功。我們與SGS Lakefield合作完成的分析表明,高品位鋰截獲證實了Li的存在。2O GRP巖牆羣中的礦牀,需要進一步深入研究。隨着我們開始2023年冬季鑽探計劃,我們期待着研究GRP地區的西北延伸,並在未來幾個月推進我們的資源擴張計劃。
GRP Dykes Swarm
玻璃鋼堤壩羣
Geology of the GRP Dykes Swarm and host rocks - The GRP dykes crosscut plutonic intrusive rocks of Monzonite composition, exhibiting medium to coarse grained Plagioclase crystals within a fine to medium grained mafic groundmass. Albitic to potassic feldspars occur frequently within the rock. The groundmass consists of amphiboles and occasional biotite. Garnet has been observed in small clusters within rare melanocratic groundmass. The Monzite has been subject to considerable seracitic and hematitic alteration, often resulting in destruction of the original plutonic minerals and giving the rock a "bleached" appearance. Small quartz and granitic Aplite dykes are common.
GRP巖牆羣和主巖的地質-GRP巖牆橫切二長巖成分的深成侵入巖,在細粒至中粒鎂鐵質基質中顯示中-粗粒斜長石晶體。鈉長石至鉀長石在巖石中經常出現。基團由角閃石和偶爾的黑雲母組成。石榴石在罕見的黑色素基質中被觀察到成小簇。二長巖經歷了大量的絹雲母和赤鐵礦的蝕變,經常導致原始深成礦物的破壞,使巖石呈現出一種“漂白”的外觀。常見的是小石英和花崗質安長巖牆。
The GRP Dykes Swarm appear to strike 110° and dip about 60-65o SSW. The mineralogy of the dykes is typical for lithium bearing pegmatite dykes, and consists of potassic feldspars, quartz, muscovite and to a lesser extent biotite, tourmaline and rare garnets and very rare beryl. The lithium bearing mineral is spodumene, which varies considerably in both grain size and distribution within the dykes. Spodumene crystals can vary in size from 1 cm to more than10+ cm in size. The GRP dykes often exhibit very large spodumene crystals, often ranging in size from 10-15 cm long. The distribution of the crystals within the dyke intersections is sporadic, with some sections containing up to 25 to 30 percent spodumene, and other sections that are spodumene poor to barren, suggesting multiple pulses of fluids and crystal mush from the parent granitic magma. The mineralogy and mineral zonation of the dyke(s) will be the subject of further study in the coming months.
GRP巖牆羣走向110°,傾角約為60-65oSSW。巖脈的礦物學特徵是典型的含鋰偉晶巖脈,由鉀長石、石英、白雲母和少量黑雲母、電氣石、稀有石榴石和非常稀有的綠柱石組成。含鋰礦物為鋰輝石,其顆粒大小和在巖牆中的分佈差異很大。鋰輝石晶體的大小從1釐米到10多釐米不等。GRP巖牆通常顯示出非常大的鋰輝石晶體,通常大小從10-15釐米長不等。在巖牆交界處,晶體的分佈是零星的,一些區段含有25%-30%的鋰輝石,另一些區段鋰輝石很少到沒有鋰輝石,這表明來自母花崗巖巖漿的多脈衝流體和晶體碎屑。堤壩的礦物學和礦物分帶將是未來幾個月進一步研究的主題。
Analytical - Half core samples are sent to SGS Lakefield for analysis. Core samples are initially crushed to a size of -12.7 mm, then fragmented to 75% passing 2mm and eventually extruded into a 250 g pulp that is pulverized to 85% passing 75 microns. Samples are sodium peroxide fused and run on ICP-AES and/or ICP- MS generating 56 element suit.
分析性-將半個巖心樣品送到SGS Lakefield進行分析。巖芯樣品最初被粉碎到-12.7 mm的尺寸,然後粉碎到75%通過2 mm,最終擠壓成250 g紙漿,粉碎到85%通過75微米。樣品經過氧化鈉熔融後,在電感耦合等離子體原子發射光譜儀和/或電感耦合等離子體質譜儀上運行,產生56種元素。
Qualified Person Statement - The information in this news release was compiled and reviewed by Dale Schultz, a Qualified Person, as defined by the Securities and Exchange Commission's S-K 1300 rules for mineral deposit disclosure, a Professional Geoscientist (P.Geo.) and a registered member of the Engineer and Geosciences of Manitoba (no. 24846) RPO (Recognized Professional Organization). Mr. Dale Schultz is the Project Manager and VP of Resource Development at Snow Lake and has sufficient experience relevant to the crystallization of lithium-cesium-tantalum (LCT) type pegmatite deposits under evaluation.
合資格人士報表-本新聞稿中的信息由符合美國證券交易委員會S-K 1300礦藏披露規則定義的合格人士Dale Schultz彙編和審查,他是一名專業地球科學家(P.Geo.)以及馬尼託巴省工程師和地球科學部(編號24846)RPO(認可專業組織)的註冊成員。Dale Schultz先生是Snow Lake的項目經理兼資源開發副總裁,在正在評估的鋰銫鉭(LCT)型偉晶巖礦牀的結晶方面擁有豐富的經驗。
Table 1.0 - List of Intercept cited in the Release
表1.0-新聞稿中引用的截獲列表
Figure 1.0 - Plan view drill hole location map of the Grass River Pegmatite Dykes Swarm
圖1.0-草河偉晶巖牆羣平面圖鑽孔位置圖
Section 1 - Cross Section of hole CBP-007
第1節-CBP-007孔的橫截面
Section 2 - Cross Section of hole CBP-018
第2節-CBP-018孔的橫截面
Section 3 - Cross Section of hole CBP-013
第3節-CBP-013孔的橫截面
Section 4 - Cross Section of hole CBP-021
第4節-CBP-021孔的橫截面
Table 2.0 - Significant Li2O% values listed in the News Release
表2.0--重要人物Li2新聞稿中列出的O%值
DDH_ID | SAMP# |
From (m) |
To (m) |
Li2O % |
SGP-001 | 54503 |
19.1 |
20.3 |
1.9 |
SGP-001 | 54505 |
20.3 |
21.3 |
1.1 |
SGP-002 | 54520 |
22.6 |
24.0 |
1.1 |
SGP-002 | 54521 |
24.0 |
24.9 |
2.0 |
SGP-002 | 54527 |
191.3 |
192.5 |
1.9 |
SGP-002 | 54529 |
192.5 |
194.0 |
1.8 |
SGP-003 | 54553 |
65.4 |
66.8 |
1.1 |
SGP-003 | 54562 |
181.5 |
183.0 |
1.1 |
SGP-003 | 54566 |
185.2 |
186.6 |
0.8 |
SGP-005 | 54596 |
18.4 |
19.0 |
2.5 |
SGP-005 | 54616 |
174.5 |
176.0 |
3.3 |
SGP-005 | 54618 |
176.0 |
177.3 |
2.3 |
SGP-007 | 54669 |
110.0 |
111.5 |
1.0 |
SGP-007 | 54671 |
111.5 |
113.0 |
1.3 |
SGP-008A | 54697 |
143.9 |
144.9 |
1.1 |
SGP-008A | 54698 |
144.9 |
146.0 |
1.1 |
SGP-008A | 54700 |
146.0 |
147.2 |
1.1 |
SGP-008A | 54826 |
147.2 |
148.8 |
1.5 |
SGP-010 | 54690 |
185.7 |
187.0 |
1.5 |
GRP-001 | 51504 |
36.0 |
37.1 |
1.5 |
GRP-001 | 51507 |
38.1 |
39.4 |
1.0 |
GRP-001 | 51511 |
41.9 |
42.9 |
0.8 |
GRP-001 | 51513 |
42.9 |
44.2 |
1.0 |
GRP-002 | 51520 |
69.0 |
70.5 |
1.2 |
GRP-002 | 51522 |
70.5 |
72.0 |
1.7 |
GRP-002 | 51523 |
72.0 |
73.5 |
0.9 |
GRP-002 | 51524 |
73.5 |
75.0 |
1.2 |
GRP-003 | 51532 |
16.0 |
17.5 |
1.8 |
GRP-003 | 51533 |
17.5 |
19.0 |
3.1 |
GRP-003 | 51535 |
19.0 |
20.5 |
3.6 |
GRP-003 | 51537 |
20.5 |
22.0 |
1.0 |
GRP-003 | 51546 |
77.1 |
78.5 |
1.5 |
GRP-003 | 51548 |
78.5 |
80.0 |
2.5 |
GRP-003 | 51550 |
80.0 |
81.5 |
1.3 |
GRP-003 | 51551 |
81.5 |
82.6 |
2.7 |
GRP-003 | 51553 |
82.6 |
83.4 |
1.0 |
GRP-004 | 51571 |
18.9 |
20.0 |
0.9 |
GRP-004 | 51573 |
20.0 |
21.5 |
1.7 |
GRP-004 | 51584 |
96.1 |
97.0 |
1.1 |
GRP-004 | 51596 |
108.2 |
109.5 |
1.4 |
GRP-004 | 51599 |
111.0 |
112.0 |
2.2 |
GRP-005 | 51617 |
30.5 |
32.0 |
1.1 |
GRP-005 | 51619 |
32.0 |
33.5 |
2.8 |
GRP-005 | 51620 |
33.5 |
35.0 |
1.3 |
GRP-005 | 51621 |
35.0 |
36.5 |
1.1 |
GRP-005 | 51622 |
36.5 |
38.0 |
1.0 |
GRP-005 | 51624 |
38.0 |
39.5 |
1.2 |
GRP-005 | 51625 |
39.5 |
41.0 |
0.9 |
GRP-006 | 51634 |
4.0 |
5.5 |
0.9 |
GRP-006 | 51635 |
5.5 |
7.0 |
2.3 |
GRP-006 | 51637 |
7.0 |
8.0 |
0.8 |
GRP-006 | 51644 |
13.1 |
14.0 |
1.0 |
GRP-006 | 51645 |
14.0 |
15.5 |
2.9 |
GRP-006 | 51647 |
15.5 |
17.0 |
2.5 |
GRP-007 | 51654 |
5.0 |
6.5 |
1.8 |
GRP-007 | 51657 |
8.0 |
9.5 |
1.2 |
GRP-007 | 51659 |
9.5 |
11.0 |
0.9 |
GRP-008 | 51755 |
69.0 |
70.0 |
1.2 |
GRP-008 | 51757 |
70.0 |
71.0 |
2.4 |
GRP-008 | 51758 |
71.0 |
72.5 |
3.4 |
GRP-008 | 51760 |
72.5 |
74.0 |
2.2 |
GRP-008 | 51761 |
74.0 |
75.5 |
1.8 |
GRP-008 | 51763 |
75.5 |
77.0 |
1.4 |
GRP-008 | 51764 |
77.0 |
77.8 |
2.4 |
GRP-008 | 51772 |
161.0 |
162.5 |
1.0 |
GRP-008 | 51773 |
162.5 |
164.0 |
1.3 |
GRP-008 | 51775 |
164.0 |
165.3 |
1.5 |
GRP-009 | 51782 |
87.5 |
89.0 |
2.1 |
GRP-009 | 51783 |
89.0 |
90.5 |
1.5 |
GRP-009 | 51785 |
90.5 |
92.0 |
1.5 |
GRP-009 | 51786 |
92.0 |
93.5 |
2.0 |
GRP-009 | 51793 |
206.9 |
208.0 |
0.9 |
GRP-009 | 51794 |
208.0 |
209.0 |
2.1 |
GRP-009 | 51795 |
209.0 |
210.5 |
1.9 |
GRP-009 | 51797 |
210.5 |
212.0 |
1.0 |
GRP-009 | 51798 |
212.0 |
213.0 |
0.9 |
GRP-010 | 51673 |
98.0 |
99.5 |
0.9 |
GRP-010 | 51675 |
99.5 |
101.0 |
1.1 |
GRP-010 | 51676 |
101.0 |
102.5 |
1.8 |
GRP-010 | 51681 |
105.5 |
107.0 |
1.3 |
GRP-010 | 51686 |
173.2 |
174.5 |
1.1 |
GRP-011 | 51706 |
110.0 |
111.5 |
1.4 |
GRP-011 | 51707 |
111.5 |
113.0 |
0.8 |
GRP-011 | 51710 |
114.5 |
116.0 |
0.9 |
GRP-011 | 51725 |
210.5 |
212.0 |
1.0 |
GRP-011 | 51728 |
213.5 |
215.0 |
1.1 |
GRP-011 | 51730 |
215.0 |
216.0 |
1.0 |
GRP-012 | 51738 |
131.0 |
132.5 |
1.7 |
GRP-012 | 51740 |
132.5 |
134.0 |
1.5 |
GRP-012 | 51741 |
134.0 |
135.5 |
2.2 |
GRP-012 | 51743 |
135.5 |
137.0 |
4.0 |
GRP-012 | 51748 |
141.5 |
143.0 |
1.4 |
GRP-012 | 51749 |
143.0 |
143.9 |
0.8 |
GRP-013 | 51810 |
125.0 |
126.5 |
2.1 |
GRP-013 | 51811 |
126.5 |
128.0 |
3.2 |
GRP-013 | 51813 |
128.0 |
129.5 |
2.0 |
GRP-013 | 51815 |
129.5 |
131.0 |
0.9 |
GRP-014 | 51822 |
103.0 |
104.0 |
1.2 |
GRP-014 | 51823 |
104.0 |
105.5 |
2.8 |
DDH_ID | 樣例編號 |
發件人(M) |
至(M) |
Li2O% |
SGP-001 | 54503 |
19.1 |
20.3 |
1.9 |
SGP-001 | 54505 |
20.3 |
21.3 |
1.1 |
SGP-002 | 54520 |
22.6 |
24.0 |
1.1 |
SGP-002 | 54521 |
24.0 |
24.9 |
2.0 |
SGP-002 | 54527 |
191.3 |
192.5 |
1.9 |
SGP-002 | 54529 |
192.5 |
194.0 |
1.8 |
SGP-003 | 54553 |
65.4 |
66.8 |
1.1 |
SGP-003 | 54562 |
181.5 |
183.0 |
1.1 |
SGP-003 | 54566 |
185.2 |
186.6 |
0.8 |
SGP-005 | 54596 |
18.4 |
19.0 |
2.5 |
SGP-005 | 54616 |
174.5 |
176.0 |
3.3 |
SGP-005 | 54618 |
176.0 |
177.3 |
2.3 |
SGP-007 | 54669 |
110.0 |
111.5 |
1.0 |
SGP-007 | 54671 |
111.5 |
113.0 |
1.3 |
SGP-008A | 54697 |
143.9 |
144.9 |
1.1 |
SGP-008A | 54698 |
144.9 |
146.0 |
1.1 |
SGP-008A | 54700 |
146.0 |
147.2 |
1.1 |
SGP-008A | 54826 |
147.2 |
148.8 |
1.5 |
SGP-010 | 54690 |
185.7 |
187.0 |
1.5 |
GRP-001 | 51504 |
36.0 |
37.1 |
1.5 |
GRP-001 | 51507 |
38.1 |
39.4 |
1.0 |
GRP-001 | 51511 |
41.9 |
42.9 |
0.8 |
GRP-001 | 51513 |
42.9 |
44.2 |
1.0 |
GRP-002 | 51520 |
69.0 |
70.5 |
1.2 |
GRP-002 | 51522 |
70.5 |
72.0 |
1.7 |
GRP-002 | 51523 |
72.0 |
73.5 |
0.9 |
GRP-002 | 51524 |
73.5 |
75.0 |
1.2 |
GRP-003 | 51532 |
16.0 |
17.5 |
1.8 |
GRP-003 | 51533 |
17.5 |
19.0 |
3.1 |
GRP-003 | 51535 |
19.0 |
20.5 |
3.6 |
GRP-003 | 51537 |
20.5 |
22.0 |
1.0 |
GRP-003 | 51546 |
77.1 |
78.5 |
1.5 |
GRP-003 | 51548 |
78.5 |
80.0 |
2.5 |
GRP-003 | 51550 |
80.0 |
81.5 |
1.3 |
GRP-003 | 51551 |
81.5 |
82.6 |
2.7 |
GRP-003 | 51553 |
82.6 |
83.4 |
1.0 |
GRP-004 | 51571 |
18.9 |
20.0 |
0.9 |
GRP-004 | 51573 |
20.0 |
21.5 |
1.7 |
GRP-004 | 51584 |
96.1 |
97.0 |
1.1 |
GRP-004 | 51596 |
108.2 |
109.5 |
1.4 |
GRP-004 | 51599 |
111.0 |
112.0 |
2.2 |
GRP-005 | 51617 |
30.5 |
32.0 |
1.1 |
GRP-005 | 51619 |
32.0 |
33.5 |
2.8 |
GRP-005 | 51620 |
33.5 |
35.0 |
1.3 |
GRP-005 | 51621 |
35.0 |
36.5 |
1.1 |
GRP-005 | 51622 |
36.5 |
38.0 |
1.0 |
GRP-005 | 51624 |
38.0 |
39.5 |
1.2 |
GRP-005 | 51625 |
39.5 |
41.0 |
0.9 |
GRP-006 | 51634 |
4.0 |
5.5 |
0.9 |
GRP-006 | 51635 |
5.5 |
7.0 |
2.3 |
GRP-006 | 51637 |
7.0 |
8.0 |
0.8 |
GRP-006 | 51644 |
13.1 |
14.0 |
1.0 |
GRP-006 | 51645 |
14.0 |
15.5 |
2.9 |
GRP-006 | 51647 |
15.5 |
17.0 |
2.5 |
GRP-007 | 51654 |
5.0 |
6.5 |
1.8 |
GRP-007 | 51657 |
8.0 |
9.5 |
1.2 |
GRP-007 | 51659 |
9.5 |
11.0 |
0.9 |
GRP-008 | 51755 |
69.0 |
70.0 |
1.2 |
GRP-008 | 51757 |
70.0 |
71.0 |
2.4 |
GRP-008 | 51758 |
71.0 |
72.5 |
3.4 |
GRP-008 | 51760 |
72.5 |
74.0 |
2.2 |
GRP-008 | 51761 |
74.0 |
75.5 |
1.8 |
GRP-008 | 51763 |
75.5 |
77.0 |
1.4 |
GRP-008 | 51764 |
77.0 |
77.8 |
2.4 |
GRP-008 | 51772 |
161.0 |
162.5 |
1.0 |
GRP-008 | 51773 |
162.5 |
164.0 |
1.3 |
GRP-008 | 51775 |
164.0 |
165.3 |
1.5 |
GRP-009 | 51782 |
87.5 |
89.0 |
2.1 |
GRP-009 | 51783 |
89.0 |
90.5 |
1.5 |
GRP-009 | 51785 |
90.5 |
92.0 |
1.5 |
GRP-009 | 51786 |
92.0 |
93.5 |
2.0 |
GRP-009 | 51793 |
206.9 |
208.0 |
0.9 |
GRP-009 | 51794 |
208.0 |
209.0 |
2.1 |
GRP-009 | 51795 |
209.0 |
210.5 |
1.9 |
GRP-009 | 51797 |
210.5 |
212.0 |
1.0 |
GRP-009 | 51798 |
212.0 |
213.0 |
0.9 |
GRP-010 | 51673 |
98.0 |
99.5 |
0.9 |
GRP-010 | 51675 |
99.5 |
101.0 |
1.1 |
GRP-010 | 51676 |
101.0 |
102.5 |
1.8 |
GRP-010 | 51681 |
105.5 |
107.0 |
1.3 |
GRP-010 | 51686 |
173.2 |
174.5 |
1.1 |
GRP-011 | 51706 |
110.0 |
111.5 |
1.4 |
GRP-011 | 51707 |
111.5 |
113.0 |
0.8 |
GRP-011 | 51710 |
114.5 |
116.0 |
0.9 |
GRP-011 | 51725 |
210.5 |
212.0 |
1.0 |
GRP-011 | 51728 |
213.5 |
215.0 |
1.1 |
GRP-011 | 51730 |
215.0 |
216.0 |
1.0 |
GRP-012 | 51738 |
131.0 |
132.5 |
1.7 |
GRP-012 | 51740 |
132.5 |
134.0 |
1.5 |
GRP-012 | 51741 |
134.0 |
135.5 |
2.2 |
GRP-012 | 51743 |
135.5 |
137.0 |
4.0 |
GRP-012 | 51748 |
141.5 |
143.0 |
1.4 |
GRP-012 | 51749 |
143.0 |
143.9 |
0.8 |
GRP-013 | 51810 |
125.0 |
126.5 |
2.1 |
GRP-013 | 51811 |
126.5 |
128.0 |
3.2 |
GRP-013 | 51813 |
128.0 |
129.5 |
2.0 |
GRP-013 | 51815 |
129.5 |
131.0 |
0.9 |
GRP-014 | 51822 |
103.0 |
104.0 |
1.2 |
GRP-014 | 51823 |
104.0 |
105.5 |
2.8 |
Table 3.0 - UTM Location, Azimuth and Dip of DDH listed in the Release.
表3.0-新聞稿中列出的DDH的UTM位置、方位和傾角。
NAD83 - UTM Zone 14 - D-GPS
NAD83-UTM 14區-D-GPS
About Snow Lake Resources Ltd.
關於雪湖資源有限公司
Snow Lake is committed to creating and operating a fully renewable and sustainable lithium mine that can deliver a completely traceable, carbon neutral and zero harm product to the North American electric vehicle and battery markets.
雪湖致力於創建和運營一個完全可再生和可持續發展的鋰礦,為北美電動汽車和電池市場提供完全可追溯、碳中性和零傷害的產品。
Our wholly owned Snow Lake LithiumTM Project now covers a 59,587-acre site that has only been 1% explored and contains an identified-to-date 11.1 million metric tonnes indicated and inferred resource at 1% Li2O.
我們全資擁有的雪湖鋰礦TM該項目目前佔地59,587英畝,僅勘探了1%,迄今已查明的1,110萬公噸已指示和推斷的資源量為1%Li2O.
Forward Looking Statements
前瞻性陳述
This press release contains "forward-looking statements" that are subject to substantial risks and uncertainties. All statements, other than statements of historical fact, contained in this press release are forward-looking statements, including without limitation statements with respect to the timing of the Meeting. We base these forward-looking statements on our expectations and projections about future events, which we derive from the information currently available to us. Forward-looking statements contained in this press release may be identified by the use of words such as "anticipate," "believe," "contemplate," "could," "estimate," "expect," "intend," "seek," "may," "might," "plan," "potential," "predict," "project," "target," "aim," "should," "will," "would," or the negative of these words or other similar expressions, although not all forward-looking statements contain these words. Forward-looking statements are based on Snow Lake Resources Ltd.'s current expectations and are subject to inherent uncertainties, risks and assumptions that are difficult to predict, including without limitation future actions by the Dissidents. Further, certain forward-looking statements are based on assumptions as to future events that may not prove to be accurate. Some of these risks and uncertainties are described more fully in the section titled "Risk Factors" in our registration statements and reports filed with the Securities and Exchange Commission. Forward-looking statements contained in this announcement are made as of this date, and Snow Lake Resources Ltd. undertakes no duty to update such information except as required under applicable law.
本新聞稿包含受重大風險和不確定因素影響的“前瞻性陳述”。除有關歷史事實的陳述外,本新聞稿中包含的所有陳述均為前瞻性陳述,包括但不限於關於會議時間的陳述。我們的這些前瞻性陳述是基於我們對未來事件的預期和預測,而這些預期和預測是從我們目前掌握的信息中得出的。本新聞稿中包含的前瞻性陳述可通過使用“預期”、“相信”、“考慮”、“可能”、“估計”、“預期”、“打算”、“尋求”、“可能”、“可能”、“計劃”、“潛在”、“預測”、“項目”、“目標”、“目標”、“應該”、“將”、“將”、“可能”、“計劃”、“潛在”、“預測”、“計劃”、“目標”、“目標”、“應該”、“將”、“可能”、“計劃”、“潛在”、“預測”、“計劃”、“目標”、“目標”、“應該”、“將”、“可能”、“可能”、“計劃”、“潛在”、“預測”、“計劃”、“目標”、“目標”、“應該”、“將”、“將“或這些詞語的否定或其他類似表述,儘管並非所有前瞻性陳述都包含這些詞語。前瞻性陳述基於雪湖資源有限公司目前的預期,受難以預測的內在不確定性、風險和假設的影響,包括但不限於持不同政見者未來的行動。此外,某些前瞻性陳述是基於對未來事件的假設,而事實可能證明這些假設並不準確。其中一些風險和不確定性在我們提交給美國證券交易委員會的註冊聲明和報告中題為“風險因素”的章節中有更詳細的描述。本公告中包含的前瞻性陳述是截至本日作出的,除適用法律要求外,雪湖資源有限公司不承擔更新此類信息的責任。
For more information, please contact:
如需更多信息,請聯繫:
media@snowlakelithium.com
ir@snowlakelithium.com
Twitter: @SnowLakeLithium
LinkedIn:
郵箱:media@nowlakelithium.com
郵箱:ir@nowlakelithium.com
推特:@SnowLakeLithium
LinkedIn:
SOURCE: Snow Lake Resources Ltd.
資料來源:雪湖資源有限公司。