The relationship between normal and strike-slip faults in Valley of Fire State Park, Nevada, and its implications for stress rotation and partitioning of deformation in the east-central Basin and Range

Author:

Aydin Atilla,de Joussineau Ghislain

Funder

DOE Basic Energy Sciences Geosciences Research Program

Publisher

Elsevier BV

Subject

Geology

Reference53 articles.

1. Permeability upscaling of fault zones in the Aztec Sandstone, Valley of Fire State Park, Nevada, with a focus on slip surfaces and slip bands;Ahmadov;Hydrogeol. J.,2007

2. The Dynamics of Faulting;Anderson,1951

3. Large-magnitude Late Tertiary Strike-slip Faulting North of Lake Mead, Nevada. U. S. Geological Survey Professional Paper 794;Anderson,1973

4. Analysis of Neogene Deformation between Beaver, Utah, and Barstow, California: Suggestions for Altering the Extensional Paradigm;Anderson,2013

5. Neogene paleostress changes in the Basin and Range: a case study at Hoover Dam, Nevada-Arizona;Angelier;Geol. Soc. Am. Bull.,1985

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