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home / news releases / REZZF - Global Battery Metals Acquires Lithium King Property in Utah


REZZF - Global Battery Metals Acquires Lithium King Property in Utah

Vancouver, British Columbia--(Newsfile Corp. - March 4, 2021) -  GBML Battery Metals Ltd. (TSXV: GBML) (FSE: REZ) (OTCQB: REZZF) (the "Company" or "GBML") is pleased to announce, that through the staking of federal placer claims, it has acquired the property area known as the Lithium King property (the "Lithium King Property" or the "Property").

Lithium King Property Highlights:

  • Prospective lithium bearing brine aquifer located on the west side of the Great Salt Lake Basin in western Utah.
  • The land position consists of approximately 7,900 acres (3,200 hectares) of placer claims.
  • Excellent infrastructure: Interstate Highway I-80 runs through the Property.
  • Adjacent to active brine mining operation.
  • Mining friendly jurisdiction.

Michael Murphy, President and CEO, commented: "We are very excited to have added the Lithium King Property to our growth-oriented portfolio of battery metals projects. Samples from the Property have recorded positive lithium values, with excellent access from Interstate Highway 80, which runs beside the Property. We look forward to rapidly advancing this Property, beginning with digitizing historical data, water sampling, modelling, and ultimately leading to drill testing."

Lithium King Property Overview

The Lithium King Property is located on the west side of the Great Salt Lake Basin in western Utah, adjacent to the community of Wendover, Utah. The land position consists of approximately 7,900 acres (3,200 hectares) of placer claims.

The Property has the potential to host a lithium, and magnesium brine deposit in an existing mineral producing location in a mining-friendly state.

Figure 1. Lithium King Property

To view an enhanced version of Figure 1, please visit:
https://orders.newsfilecorp.com/files/7080/76037_figure%201%20jpeg.jpg

The lithium and magnesium on the Lithium King Property are present as dissolved salts in a large surface brine aquifer, which is believed to be derived from both surface erosion of lithium-rich rhyolites (as part of the Pilot and Toano Ranges) and mineral-rich geothermal brine flows into the basin sediments from deep seated faults underlying the 20-mile-long basin.

Lithium values from several samples from 39 shallow wells (25 feet) averaged 244 parts per million (ppm) and ranged from a low 49 ppm to a high of 1,200 ppm. The lithium values from these wells are set out in Schedule A. (See also United States Geological Survey Data Base: Produced Waters, Volume 2.2n.xlsx, available in the Utah Geological Survey files.) The Lithium King Property is within the Great Basin of the western United States, where lithium concentrations of greater than 10 ppm in brines are anomalous. Lithium values from the only lithium production in the United States, in Clayton Valley, Nevada, also in the Great Basin, range from 75 to about 250 ppm. (PC - W. R. Henkle, Jr.).

Figure 2. Property looking north towards Pilot Peak

To view an enhanced version of Figure 2, please visit:
https://orders.newsfilecorp.com/files/7080/76037_96f502bde4881a7a_007full.jpg

Magnesium values at the Property and near vicinity range between 1,300 and 8,500 ppm (see United States Geological Survey Data Base: Produced Waters, Volume 2.2n.xlsx, available in the Utah Geological Survey (USGS) files, and Selected Ground-Water Data, Bonneville Salt Flats and Pilot Valley, Western Utah, Utah Basic-Data Release No. 30, United States Geological Survey).

The shallow aquifer water samples (as per USGS sampling) may not reflect the deeper basin below 25 feet depth. Drilling to bedrock and brine sampling is needed to confirm the presence of and concentration of lithium in the deeper basin brines.

In addition to the large surface brine aquifer, several deeper, thick, porous clastic horizons are present. These horizons were identified by inspection of the drill logs from the Shell-Salduro oil exploration well which was drilled just west of the Property boundary. The historical drill logs identified this deep sequence of aquifers (greater than 70% volcanic conglomerates) at the basin bedrock contact, at a depth of between 1,350 and 2,650 feet, beneath 1,300 feet of impervious, clay-rich sediments. They provide posited permeable reservoirs for large quantities of what are thought to be higher value brines (undiluted by meteoritic water). Because of the moderate target depths, both exploration and production drilling could be undertaken with conventional hard rock drilling equipment and should not require oilfield tools.

The lithium and magnesium anomalous area overlies basement faulting identified by geophysical surveying and confirmed by oil and gas drilling records (the logs of the Shell-Salduro oil exploration well located in the Property vicinity, are public information, maintained by the Utah Dept. of Oil, Gas and Mining). The geothermal fluids which are thought to be sourced from the underlying faults are believed to be the primary source of mineralization. This is supported by: (1) the U.S. Geological Survey observation that, despite the presence of an industrial minerals extraction operation in an adjacent area for many years, there has been no depletion of mineral values as would be expected if the recharge to the aquifer was from meteoric waters (USGS Professional Paper # 1585); and (2) water temperatures are elevated over the highly mineralized area (see Selected Ground-Water Data, Bonneville Salt Flats and Pilot Valley, Western Utah, Utah Basic-Data Release No. 30, United States Geological Survey and, United States Geological Survey Data Base: Produced Waters, Volume 2.2n.xlsx, available in the Utah Geological Survey files).

Work Program

To assess the lithium potential of the basin brines on the Lithium King Property and subject to the receipt of any required drilling permits, GBML expects to conduct the following work:

  1. Locate and digitize existing oil well data to help in the modelling of the basin.
  2. Acquire public domain geophysical datasets. This will help in improving the subsurface structural and geological model. A depth to basement modelling exercise shall be completed. The data to be included in such model is expected to include, but is not limited to:
    • Gravity
    • Magnetics
    • Seismic
    • Exploration mud rotatory drilling with wireline geophysics to evaluate the stratigraphy and basement depth for the Property area.
  1. Water sampling of drill holes using in-hole packer equipment to test for lithium enrichment and deleterious element content of the brine.
  2. Acquire additional geophysical data to assess basement depth, water content and brine depth throughout the basin. This will be completed by a combination of gravity and electro magnetic data acquisition.
  3. Further drilling to test for:
    •  Stratigraphy
    • Brine composition
    • Production metrics

Finder's Fee

In connection with acquiring the Property, the Company has agreed to pay a finder's fee (the "Finder's Fee") to Atherton Resources LLC. Subject to acceptance of the TSX Venture Exchange, the Finder's Fee shall include: (1) a 2% net smelter royalty over the Property, with a right to repurchase 1% of such royalty for the greater of US$1 million or 10% of the value of such 1% royalty; (2) the issuance of 150,000 common shares ("Shares") of the Company upon delivery of a technical report prepared in accordance with National Instrument 43-101 in respect of the Property; and (3) the issuance of 380,000 Shares upon delivery of a positive feasibility study in respect of the Property.

Qualified Person

The scientific and technical information in this news release has been reviewed and approved by William R. Henkle, Jr., a "qualified person" within the meaning of National Instrument 43-101.

About Global Battery Metals Ltd.

GBML is a mineral exploration company with a focus on metals that make up and support the rapid evolution to battery power. GBML's common shares are listed on the TSX Venture Exchange, OTCBB and Frankfurt. GBML currently has two projects: (1) an option to acquire up to 90 per cent of the North-West Leinster lithium property in Ireland, and (2) a 55-per-cent stake in Peru-based Lara copper property, which has over 10,000 metres of drilling. As previously disclosed, Minsur S.A., a Peruvian mining company, entered into an option agreement with GBML and Lara Exploration Ltd. to acquire the Lara property for staged payments of $5.75 million (U.S.). GBML will retain a 0.75-per-cent net smelter royalty.

Michael Murphy BA, MBA, MSc., ICD
President & CEO
E:
MM@gbml.ca

Cautionary Note Regarding Forward-Looking Statements

This press release contains forward-looking information within the meaning of the applicable Canadian securities legislation. Forward-looking information in this press release includes, but is not limited to, statements about the Lithium King Property, including the potential lithium values of the brine, the lithium potential of the Property, the receipt of required drilling permits and the proposed work program, the terms of the Finder's Fee and regulatory approval of such fee. These statements are based on information currently available to the Company and the Company provides no assurance that actual results will meet management's expectations. Sufficient work has not been performed on the Lithium King Property to determine what lithium and potassium values are present. In certain cases, forward-looking information may be identified by such terms as "anticipates", "believes", "could", "estimates", "expects", "may", "shall", "will", or "would". These forward-looking statements are subject to numerous risks and uncertainties, certain of which are beyond the control of the Company, including, but not limited to, impacts arising from the global disruption caused by the COVID-19 coronavirus outbreak, fluctuations in general macroeconomic conditions, availability of financing, the potential for gold and/or lithium at any of the Company's properties, the prospective nature of any claims comprising the Company's property interests, industry conditions, dependence upon regulatory approvals, and uncertainty of sample results, timing and results of future exploration. Please refer to the Company's MD&A for the year ended April 30, 2020 and other disclosure documents filed under its profile on SEDAR for other risks that could materially affect the Company. These and other factors should be considered carefully, and readers should not place undue reliance on the Company's forward-looking information. The Company does not undertake to update any forward-looking information that may be made from time to time by the Company or on its behalf, except in accordance with applicable securities laws.

NEITHER THE TSX-V NOR ITS REGULATION SERVICES PROVIDER (AS THAT TERM IS DEFINED IN THE POLICIES OF THE TSX-V) ACCEPTS RESPONSIBILITY FOR THE ADEQUACY OF THIS RELEASE. NO STOCK EXCHANGE, SECURITIES COMMISSION OR OTHER REGULATORY AUTHORITY HAS APPROVED OR DISAPPROVED THE INFORMATION CONTAINED HEREIN.

Schedule A

LITHIUM KING PLAY AREA SHALLOW AQUIFER BRINES
TOOELE COUNTY, UTAH
PREPARED BY: Henkle and Assoc. from the U.S. Geologicial Survey Database: Produced Waters, Volume 2.2n.xlsx
COUNT
WELLNAME
Li
Mg
Mg/Li
Ca
Ca/Li
Ca/Mg
WELLTYPE
WELLCLASS
1
NWIS Well (C- 1-17)18cab- 1
1200
5600
4.6666667
1000
0.83333333
0.178571429
Geothermal

2
NWIS Well (B- 1-17)22abd- 1
1100
5400
4.9090909
1000
0.90909091
0.185185185
Geothermal

3
NWIS Well (B- 1-17)29dac- 1
1000
5400
5.4
940
0.94
0.174074074
Geothermal

4
NWIS Well (C- 1-18) 3dcd- 2
970
4800
4.9484536
1000
1.03092784
0.208333333
Geothermal

5
NWIS Well (B- 1-17)11aac- 1
810
5000
6.1728395
1200
1.48148148
0.24
Geothermal











6
NWIS Well (C- 1-17) 4bba- 1
810
4300
5.308642
940
1.16049383
0.218604651
Geothermal

7
NWIS Well (B- 1-17)22bca- 1
760
4500
5.9210526
920
1.21052632
0.204444444
Geothermal

8
NWIS Well (B- 1-17)12dcc- 1
730
4700
6.4383562
1200
1.64383562
0.255319149
Geothermal

9
NWIS Well (B- 2-17)36ddd- 1
720
4600
6.3888889
1200
1.66666667
0.260869565
Geothermal

10
NWIS Well (B- 1-17)23bad- 2
700
4300
6.1428571
1200
1.71428571
0.279069767
Geothermal











11
NWIS Well (B- 1-17)19dad- 2
620
3700
5.9677419
1100
1.77419355
0.297297297
Geothermal

12
NWIS Well (B- 1-17)23abd- 1
580
3800
6.5517241
1300
2.24137931
0.342105263
Geothermal

13
NWIS Well (B- 1-17)22aad- 1
570
4100
7.1929825
1100
1.92982456
0.268292683
Geothermal

14
NWIS Well (C- 1-18)17bdb- 1
420
3100
7.3809524
1100
2.61904762
0.35483871
Geothermal

15
NWIS Well (B- 1-17)21add- 3
290
3000
10.344828
1200
4.13793103
0.4
Geothermal











16
NWIS Well (C- 1-17)15dbd- 1
250
1800
7.2
1100
4.4
0.611111111
Geothermal

17
NWIS Well (C- 1-18)11ccd- 1
170
1800
10.588235
1200
7.05882353
0.666666667
Geothermal

18
NWIS Well (C- 3- 2)35abc- 1
120
8500
70.833333
910
7.58333333
0.107058824
Geothermal

19
NWIS Well (C- 1-17)18cab- 1
95
5100
53.684211
960
10.1052632
0.188235294
Geothermal

20
NWIS Well (B- 4-18)17ddd- 1
88
2500
28.409091
2200
25
0.88
Geothermal











21
NWIS Well (B- 1-17)29dac- 1
88
4800
54.545455
830
9.43181818
0.172916667
Geothermal

22
NWIS Well (C- 1-17)17bba- 1
86
5000
58.139535
970
11.2790698
0.194
Geothermal

23
NWIS Well (C- 1-18)11ccd- 2
85
4300
50.588235
1100
12.9411765
0.255813953
Geothermal

24
NWIS Well (B- 4-18)17aaa- 1
85
3700
43.529412
1000
11.7647059
0.27027027
Geothermal

25
NWIS Well (C- 2- 1) 6abc- 4
84
5700
67.857143
920
10.952381
0.161403509
Geothermal











26
NWIS Well (B- 5-18)32ddc- 1
81
2500
30.864198
2200
27.1604938
0.88
Geothermal

27
NWIS Well (B- 4-18)17ddd- 1
78
2900
37.179487
2500
32.0512821
0.862068966
Geothermal

28
NWIS Well (B- 5-18)32ddc- 1
78
3100
39.74359
2900
37.1794872
0.935483871
Geothermal

29
NWIS Well (C- 1-17) 4bba- 1
75
4700
62.666667
1000
13.3333333
0.212765957
Geothermal

30
NWIS Well (C- 3- 5) 4bbb- 2
75
5300
70.666667
1100
14.6666667
0.20754717
Geothermal











31
NWIS Well (B- 1-17)31acc- 1
72
5700
79.166667
1100
15.2777778
0.192982456
Geothermal

32
NWIS Well (C- 1-17)17bba- 1
71
5200
73.239437
1000
14.084507
0.192307692
Geothermal

33
NWIS Well (B- 1-17)31acc- 1
71
5100
71.830986
910
12.8169014
0.178431373
Geothermal

34
NWIS Well (B- 1-17)11aac- 1
69
3800
55.072464
970
14.057971
0.255263158
Geothermal

35
NWIS Well (B- 1-17)31acc- 1
69
5800
84.057971
1100
15.942029
0.189655172
Geothermal











36
NWIS Well (B- 2- 1)24bad-10
69
2400
34.782609
2200
31.884058
0.916666667
Geothermal

37
NWIS Well (B- 1-17)12dcc- 1
67
2200
32.835821
2100
31.3432836
0.954545455
Geothermal

38
NWIS Well (B- 1-17)22abd- 1
67
4300
64.179104
970
14.4776119
0.225581395
Geothermal

39
NWIS Well (B- 4-18) 1cbc- 1
66
2200
33.333333
2000
30.3030303
0.909090909
Geothermal

40
NWIS Well (C- 3- 5) 5aba- 1
66
4400
66.666667
1100
16.6666667
0.25
Geothermal











41
NWIS Well (C- 1-18) 6adc- 2
65
1400
21.538462
1200
18.4615385
0.857142857
Geothermal

42
NWIS Well (D- 1- 1) 4cac- 1
63
4000
63.492063
1200
19.047619
0.3
Geothermal

43
NWIS Well (B- 1-17)36dac- 1
63
4800
76.190476
1100
17.4603175
0.229166667
Geothermal

44
NWIS Well (B- 1-17)26cad- 1
61
4700
77.04918
1100
18.0327869
0.234042553
Geothermal

45
NWIS Well (C- 2- 1)34dda- 1
61
3900
63.934426
1100
18.0327869
0.282051282
Geothermal











46
NWIS Well (B- 1-17)31acc- 3
60
3900
65
1100
18.3333333
0.282051282
Geothermal

47
NWIS Well (C- 1-18)17bdb- 1
60
3300
55
1100
18.3333333
0.333333333
Geothermal

48
NWIS Well (B- 1-18)32ccc- 1
59
1300
22.033898
920
15.5932203
0.707692308
Geothermal

49
NWIS Well (B- 1-17)34ddd- 1
59
4200
71.186441
1000
16.9491525
0.238095238
Geothermal

50
NWIS Well (B- 1-17)31acc- 2
59
4400
74.576271
950
16.1016949
0.215909091
Geothermal











51
NWIS Well (B- 1-17)31acc- 3
57
3300
57.894737
1000
17.5438596
0.303030303
Geothermal

52
NWIS Well (B- 2-17)36ddd- 1
56
3400
60.714286
1200
21.4285714
0.352941176
Geothermal

53
NWIS Well (B- 1-17)31acc- 2
54
4500
83.333333
1000
18.5185185
0.222222222
Geothermal

54
NWIS Well (B- 4-18)33ccc- 1
54
1700
31.481481
2100
38.8888889
1.235294118
Geothermal

55
NWIS Well (C- 1-17)10aac- 1
53
3500
66.037736
1200
22.6415094
0.342857143
Geothermal











56
NWIS Well (B- 1-17)26cad- 1
52
3200
61.538462
1200
23.0769231
0.375
Geothermal

57
NWIS Well (A- 3- 2)26aab- 1
51
3400
66.666667
1100
21.5686275
0.323529412
Geothermal

58
NWIS Well (B- 1-17)23abd- 1
50
3200
64
1300
26
0.40625
Geothermal

59
NWIS Well (B- 4-18)33ccc- 1
50
2200
44
2600
52
1.181818182
Geothermal

60
NWIS Well (B- 1-17)31acc- 2
49
4600
93.877551
1000
20.4081633
0.217391304
Geothermal

 

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/76037

Stock Information

Company Name: Redzone Resources
Stock Symbol: REZZF
Market: OTC
Website: gbml.ca

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