VANCOUVER, British Columbia, Oct. 09, 2018 (GLOBE NEWSWIRE) -- MGX Minerals Inc. (“MGX” or the
“Company”) (CSE: XMG / OTCQB: MGXMF / FSE: 1MG) is pleased to announce it has signed the Definitive Option Agreement, after completing
the due diligence in relation to the Memorandum of Understanding dated August 8th 2018, to acquire 50% of the issued
shares of Chilean Lithium Salars SpA (“CLS”). CLS is a wholly owned subsidiary of Chilean Lithium Salars Pty Ltd. (“CLSH”) and
holds a 100% interest in three prospective lithium exploration Projects (the “Projects”) located in Chile, including Francisco
Basin, Laguna Brava and Laguna Escondida Lithium Projects.
Two samples from the Laguna Brava Project were received at PurLucid Treatment Solutions Inc. (“PurLucid”) facilities in Calgary,
Alberta to undergo pilot testing to prepare a Rapid Lithium Extraction unit deployment. Drilling contractors will be on site this
week to prepare the drilling program at Francisco Basin Project, which will be overseen by SRK Consulting to deliver a 43-101
complaint Resource Estimation as soon as the exploration program is completed.
Following the positive response from the Chilean state agency National Geology and Mining Service (“SERNAGEOMIN”) and the
Environmental Assessment Service (“SEA"), the Company plans to ship a rapid lithium brine system shortly. The Special Lithium
Operation Contract “CEOL”, is a requirement to carry any lithium related commercial activity in Mining Concessions granted after
1983.
Francisco Basin Lithium Project
The Francisco Basin lithium project (“Francisco Basin”) is located 30km south of Maricunga salar, 100 km southeast of the regional
center of Copiapo and accessible via a regional highway and established tracks. The lease area comprises 12,900 hectares.
Historical exploration work on the project was previously limited to hydrology studies. In January 2018, CLSH completed a
reconnaissance brine sampling at the project. This sampling confirmed the presence of lithium enrichment in the surface brines. The
samples were assayed at the University of Antofagasta (“Antofagasta”), Antofagasta, Chile which has one of the two leading
laboratories in the world for this type of brine analysis. In May 2018, sampling continued and a 2.5L sample was taken near the
southern shore of the surface Northern lagoon and sent to Servicios Quimicos Ltda. (“SERQUIM”), Antofagasta, Chile for content
analysis. CLSH reported results to date are shown in Table 1.
A geophysical program comprising an electromagnetic survey was completed in April 2018. The survey was based on a grid of
sections which indicated the presence of high conductivity brines in two zones with significant thickness and horizontal coverage.
The presence of anomalous lithium levels in the water body area located in the Northern lagoon, which is potentially underlain by a
fault bound, saturated basin of undetermined thickness and the presence of widespread felsic to intermediate volcanic rocks as a
lithium source.
Table 1. Francisco Basin Assay Samples
Sample |
Na g/L |
K g/L |
Li ppm |
Mg g/L |
SO4 g/L |
B ppm |
Dens |
Northern Lagoon - January 2018 |
LNF
01 |
75.2 |
4.59 |
372 |
2.00 |
4.07 |
799 |
1.179 |
LNF
02 |
72.5 |
4.34 |
372 |
1.92 |
4.07 |
832 |
1.170 |
LNF
03 |
69.5 |
4.06 |
369 |
1.85 |
3.74 |
767 |
1.163 |
LNF
04 |
74.5 |
4.32 |
374 |
1.75 |
4.02 |
832 |
1.174 |
LNF
05 |
80.0 |
4.40 |
388 |
1.78 |
4.71 |
961 |
1.188 |
LNF
06 |
67.9 |
3.98 |
361 |
1.73 |
3.85 |
821 |
1.181 |
LNF
07 |
79.8 |
4.66 |
387 |
1.74 |
4.44 |
864 |
1.183 |
LNF
08 |
73.4 |
4.31 |
371 |
1.86 |
3.93 |
842 |
1.172 |
LNF
09 |
76.8 |
4.39 |
374 |
1.70 |
4.05 |
864 |
1.174 |
LNF
10 |
80.0 |
4.56 |
384 |
1.86 |
4.38 |
896 |
1.185 |
Northern Lagoon - May 2018 |
LNF
01 |
103.0 |
6.62 |
694 |
3.54 |
28.70 |
- |
- |
Southern Lagoo - January 2018 |
LNF
11 |
2.35 |
0.19 |
7.9 |
0.15 |
3.07 |
248 |
1.007 |
LNF
12 |
0.57 |
0.41 |
3.0 |
0.003 |
1.55 |
151 |
1.121 |
LNF
13 |
1.27 |
0.01 |
0.4 |
0.07 |
0.61 |
65 |
1.002 |
The Francisco Basin salar is within a large, fault-bound, alluvium-filled basin to the immediate south of the Copiapo Volcano.
The basin is closed, drains a large area and the salar appears to be the lowest point within the drainage.
The rocks in the drainage surrounding this salar are dominantly volcanic, ranging in age from Eocene to Miocene, juxtaposed with
some older rocks. To the west is a Cretaceous sedimentary sequence separated from the volcanic rocks of the Francisco Basin area by
the Cerro Guerrita Fault. To the east, an older Oligocene to Miocene volcanic sequence is overlain by the Copiapo volcanic
rocks.
The Francisco Basin alluvial basin sits at the junction of three catchments. These river systems presumably provide the fill for
the basin and are in part, along with the limits of the salar, structurally controlled. The alluvial fill may be covering
post-Copiapo aged faulting.
Laguna Brava Project
The Laguna Brava salar (“Laguna”) is geologically prospective for lithium brine. The catchment is large and dominated by volcanic
rocks, many of which have been altered by hydrothermal fluids associated with volcanism. The lake is also fed by active hot
springs. Historical sampling of surface brines indicated significant lithium enrichment. In December 2017, CLSH undertook a
four-hole reconnaissance drilling program at a southern access point of the salar to investigate the deeper aquifer. Prior to the
CLSH reconnaissance drilling program in December 2017, no previous work had been undertaken to assess the volume and grade of the
subsurface resource. Previous work recommended that the subsurface brines be investigated on the basis of his conclusion that
Laguna Brava is geothermally fed. The presence of hot springs being present either at the margins or beneath salars is common
within the Chilean Altiplano, other notable locations include the Salar de Coposa in Region I and Salar de Atacama in Region II.
The principal origin of lithium in the Salar de Atacama is interpreted to be the lithium-bearing geothermal waters from the El
Tatio Geyser Field, located north of the salar. The geothermal fluids enter the northern part of the Salar de Atacama via surface
and subsurface flow. It has also been reported that the chemistry of the salar brines is almost identical to the chemistry of the
geothermal fluids of El Tatio.
Furthermore, work by Risacher et al., (2003) has shown that subsurface brines contained within the volcanic geology are of a
much higher concentration, typically 250,000–350,000 mg/L TDS. Given this hypothesis, CLSH commissioned a reconnaissance drilling
program in December 2017 comprising four bores; the locations are shown in Figure 6-4. Two bores reached the design depth of 120 m,
and the other two bores were abandoned due to collar collapse because of high water flows. The results from this program confirmed
the presence of lithium at depth. Results were as follows (Sanchez, 2018):
Table 2. Assay Results from Reconnaissance Drilling
Bore |
No. of
Samples |
Li
(mg/L) |
Na
(mg/L) |
K
(mg/L) |
Mg
(mg/L) |
So4
(mg/L) |
B
(mg/L) |
Density |
LBRC001 |
5 |
190 |
31860 |
1842 |
1453 |
8726 |
504 |
1.066 |
LBRC002 |
11 |
167 |
28376 |
1635 |
1175 |
8189 |
494 |
1.058 |
LBRC003 |
24 |
184 |
30979 |
1730 |
1288 |
8995 |
536 |
1.064 |
LBRC004 |
16 |
201 |
34059 |
1999 |
1587 |
8513 |
519 |
1.071 |
Average |
185 |
31,320 |
1800 |
1375 |
8605 |
515 |
1.065 |
A geophysical program comprising electromagnetic and gravity surveys was completed by CLSH in February 2018. The
electromagnetic survey based on sections around the periphery of the salar indicated the presence of high conductivity brines
exceeding 100 meter thickness at the margins of the salar. The survey indicated that drill holes completed prior to the program
were in an area with brines of relatively low conductivity.
Within the vicinity of the Laguna Brava salar, the Project includes additional concessions covering Lagunas del Gilguero and the
southern margin of Piedra Parada.
Laguna Escondida Salar
The Laguna Escondida project (“Laguna Escondida “) is located approximately 200 km east–northeast of the regional capital and is
accessible via a provincial highway to within 10–15 km of the project.
Regional Geology
The Portfolio of projects are located within the Central Volcanic Zone in the foothills of the Andes mountain range on the eastern
side of Chile. All the projects are located at altitudes exceeding 4,000 m. The geology of this region, like the rest of Chile, is
dominated by the eastward subduction zone under the entire country generating uplift that has created the Andes Mountains and the
Coastal Cordillera (Moreno and Gibbons, 2007). This subduction has intensely deformed the older rocks and generated volcanic
activity that spans geological history from the Mesozoic to the present.
Terms of the Option Agreement
To acquire an undivided 50% interest in CLS, MGX has agreed to make Option Payments totaling US$1.5 million. The first US$100,000
portion of the Option Payments are payable in cash at the discretion of CLS while the remainder of Options Payments will be payable
in common shares of the Company. MGX has agreed to incur exploration expenditures totaling US$2 million and also complete an NI
43-101 resource estimate on at least one of the Projects no later than 20 months after the Effective Date of the MOU. MGX will act
as project operator and appoint Mr. Aldo Boitano, current project manager for CLS, as project manager to work alongside Kura
Minerals. CLSH shall contribute an equal amount of expenditures to maintain its respective interest in CLS. MGX also maintains the
right to participate as a service provider of the engineering, construction and/or procurement of a brine processing plant using
its rapid lithium extraction technology. Closing of the transaction remains subject to due diligence.
Rapid Lithium Brine Extraction Technology
MGX has developed a rapid lithium extraction technology eliminating or greatly reducing the physical footprint and investment in
large, multi-phase, lake sized, lined evaporation ponds, as well as enhancing the quality of extraction and recovery across a
complex range of brines as compared with traditional solar evaporation. This technology is applicable to petrolithium (oil and gas
wastewater), natural brine, and other brine sources such as lithium-rich mine and industrial plant wastewater. The technology was
recently chosen as winner of the Base and Specialty Metals Industry Leadership Award at the 2018 S&P Global Platts Global
Metals Awards, held in London in May (see press release dated May 18, 2018).
Qualified Person
Andris Kikauka (P. Geo.), Vice President of Exploration for MGX Minerals, has prepared, reviewed and approved the scientific and
technical information in this press release. Mr. Kikauka is a non-independent Qualified Person within the meaning of National
Instrument 43-101 Standards.
About MGX Minerals
MGX Minerals is a diversified Canadian resource company with interests in advanced material and energy assets throughout North
America. Learn more at www.mgxminerals.com.
Contact Information
Jared Lazerson
President and CEO
Telephone: 1.604.681.7735
Web: www.mgxminerals.com
Neither the Canadian Securities Exchange nor its Regulation Services Provider (as that term is defined in the policies of
the Canadian Securities Exchange) accepts responsibility for the adequacy or accuracy of this release.
Forward-Looking Statements
This press release contains forward-looking information or forward-looking statements (collectively
"forward-looking information") within the meaning of applicable securities laws. Forward-looking information is typically
identified by words such as: "believe", "expect", "anticipate", "intend", "estimate", "potentially" and similar expressions, or are
those, which, by their nature, refer to future events. The Company cautions investors that any forward-looking information provided
by the Company is not a guarantee of future results or performance, and that actual results may differ materially from those in
forward-looking information as a result of various factors. The reader is referred to the Company's public filings for a more
complete discussion of such risk factors and their potential effects which may be accessed through the Company's profile on SEDAR
at www.sedar.com.
Photos accompanying this announcement are available at
http://www.globenewswire.com/NewsRoom/AttachmentNg/ba7b1745-b0b7-44c7-819e-1935d2011a59
http://www.globenewswire.com/NewsRoom/AttachmentNg/ddd7bf2d-e5b0-4c8d-a632-15f03a10c20c