Controls on fault-zone architecture in poorly lithified sediments, Rio Grande Rift, New Mexico: Implications for fault-zone permeability and fluid flow-Reference-Cited by-同舟云学术

Controls on fault-zone architecture in poorly lithified sediments, Rio Grande Rift, New Mexico: Implications for fault-zone permeability and fluid flow

Published:1999 Issue: Volume: Page:27-49
ISSN:0065-8448
Container-title:Faults and Subsurface Fluid Flow in the Shallow Crust
language:
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Author:

Heynekamp Michiel R.,Goodwin Laurel B.,Mozley Peter S.,Haneberg William C.

Publisher

American Geophysical Union

Reference53 articles.

1. Cataclastic rocks of the San Gabriel fault - An expression of deformation at deeper crustal levels in the San Andreas fault zone;Anderson;Tectonophysics,1983

2. Region 7, Central alluvial basins;Anderson,1988

3. Effect of faulting on fluid flow in porous sandstones: petrophysical properties;Antonellini;Amer. Assoc. Petrol. Geol. Bull.,1994

4. Effect of faulting on fluid flow in porous sandstones: geometry and spatial distribution;Antonellini;Amer. Assoc. Petrol. Geol. Bull.,1995

5. Small faults formed as zones of deformation bands and as slip surfaces in sandstone;Aydin;Pure Appl. Geophys.,1978

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