Muddy Mountain Project Area - Highly Enriched In Lithium, page-44

FYI... More current data

Late Cenozoic displacement transfer in the eastern Sylvania Mountain fault system and Lida Valley pull-apart basin, southwestern Nevada, based on three-dimensional gravity depth inversion and forward models

1. Sarah B. Dunn*,
2. John S. Oldow and
3. Nicholas J. Mueller

2015 Geological Society of America
http://geosphere.gsapubs.org/content/11/5/1565.abstract

In 2012 and 2013 a geological research team led by Dr. John Oldow of the University of Texas, Dallas collected approximately 500 gravity measurements along 7 transects crossing the Lida Valley.

The detailed gravity survey results indicate strong gravity lows within two, faulted sub-basins approximately 7 kilometres (4.5 miles) apart, each interpreted to be hundreds of metres deep.
The Lida Valley is a flat, desert basin with a similar geological setting to the established Clayton Valley basin, which hosts North America's only producing lithium mine at Silver Peak, located 40 kilometres (26 miles) to the northwest.









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AND this....

In February and March 2016, Nevada Sunrise received results from two TDEM surveys carried out at Gemini. The moving-loop TDEM surveys over Gemini West and Gemini East detected conductive zones within the sub-basins defined by Dr. Oldow’s gravity surveys. The results gained from the TDEM survey are interpreted to be conductive brines at depth located well below the non-conductive alluvium (sediments) at surface.

A conductive layer 150-250 metres deep appears to cover most of Gemini West and Gemini East, and several isolated strong conductive zones were interpreted at depths from 400 to 600 metres.
The conductive layers and zones are indicative of brine solutions in porous aquifers and traps within each sub-basin.




http://www.nevadasunrise.ca/projects/nevadalithium/