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Tectonics of the Eastern Great Basin. Tyler Szwarc and Mark Gorenc. The Great Salt Lake Basin. Bounded by normal faults that reach up down to 5 km into the crust. Cenozoic sediments fill the grabens up to 10,000 feet.
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Tectonics of the Eastern Great Basin Tyler Szwarc and Mark Gorenc
The Great Salt Lake Basin • Bounded by normal faults that reach up down to 5 km into the crust. • Cenozoic sediments fill the grabens up to 10,000 feet. • Cenozioc sediments include sandstone, siltstone, conglomerates, tuffs, and salt deposits. • The GSL is located on top of Cenozoic sediments and above several normal faults.
Willis 2005 A’ A A’ A Krygier
Seismic profile across Great Salt Lake Viveiros 1986