Internal structure, fault rocks, and inferences regarding deformation, fluid flow, and mineralization in the seismogenic Stillwater normal fault, Dixie Valley, Nevada-Reference-Cited by-同舟云学术

Internal structure, fault rocks, and inferences regarding deformation, fluid flow, and mineralization in the seismogenic Stillwater normal fault, Dixie Valley, Nevada

Published:2010-11 Issue:11 Volume:32 Page:1576-1589
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Caine Jonathan Saul,Bruhn Ronald L.,Forster Craig B.

Publisher

Elsevier BV

Subject

Geology

Reference83 articles.

1. Effect of faulting on fluid flow in porous sandstones; petrophysical properties;Antonellini;AAPG Bulletin,1994

2. Anatomy of a normal fault with shale smear; implications for fault seal;Aydin;AAPG Bulletin,2002

3. Fracture permeability and its relationship to in-situ stress in the Dixie Valley, Nevada, geothermal reservoir;Barton,1997

4. Structural and fluid-chemical properties of seismogenic normal faults; earthquake source processes;Bruhn,1990

5. Fracturing and hydrothermal alteration in normal fault zones; faulting, friction, and earthquake mechanics; part 1;Bruhn;Pure and Applied Geophysics,1994

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