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CARACHI PAMPA PROJECT

PROJECT ZONE
RESOURCES ESTIMATION

It has resources estimated for 4.4 millions tons equivalent to Lithium Carbonate (LCE) at permeable sediments level.

In 2017 the drilling performed confirmed the presence of a zone of brines under the alluvial cover in the basin surface. The salt lake is in an intersection with a depth of 140 m and samples has been taken at 183 to 198 m depth and had given a an average result of 229 mg/l Lithium. An Electronic Vertical Sondage (VES) with geological features suggests that the zone of brines is at a depth even inferior in zones where next drilling are going to be performed.

VES results allow to differentiate four main zones in what regards geo-electrical issues:

Unit 1: A zone in the upper section shows resistivity values relatively high among 95 to 700 ohm. Probably, this zone is a dry unit composed with gravier and sand with a small amount of clay and failles.

Unit 2: A semi restrictive layer that have values among 50 to 180 ohm/m. Probably, this zone  is composed by sand and gravier with clean waters and other salties. The thickness of this unit goes from 11 to 127 m.

Unit 3: A semi-conductive zone that shows resistance 

PRELIMINAR STUDIES PERFORMED

The studies carried out in the mining claims of this project, were realized by the known geologist Dr. Schalamuck, who determined that those claims present a prospective interest and a new  mining-geological state of studies is supposed:

Stage 1: A geophysical prospection by 15  VES in each claim.

Unit 2: A semi restrictive layer that have values among 50 to 180 ohm/m. Probably, this zone  is composed by sand and gravier with clean waters and other salties. The thickness of this unit goes from 11 to 127 m.

Unit 3: A semi-conductive zone that shows a resistivity among 27 to 33 omh/m. It can be interpreted as a mix zone that holds salty waters and brines. It is restrained to the South-West corner.

Unit 4: A highly conductive zone that seems to cover an extensive layer. Resistivity values goes from 0.1 to 1.4 ohm/m. The high response in this zones holds the interpretation given that says that this zones hold brines.

GEO-ELECTRICAL STUDY

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