Flow and transport effects of compaction bands in sandstone at scales relevant to aquifer and reservoir management

Author:

Sternlof K. R.1,Karimi-Fard M.2,Pollard D. D.1,Durlofsky L. J.2

Affiliation:

1. Department of Geological and Environmental Sciences; Stanford University; Stanford California USA

2. Department of Petroleum Engineering; Stanford University; Stanford California USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference42 articles.

1. Effect of faulting on fluid flow in porous sandstones: Petrophysical properties;Antonellini;AAPG Bull.,1994

2. Petrophysical study of faults in sandstone using petrographic image analysis and x-ray computerized tomography;Antonellini;Pure Appl. Geophys.,1994

3. Small faults formed as deformation bands in sandstone;Aydin;Pure Appl. Geophys.,1978

4. Analysis of faulting in porous sandstones;Aydin;J. Struct. Geol.,1983

5. Mesozoic and Cenozoic tectonic development of the Muddy, North Muddy, and northern Black Mountains, Clark County, Nevada;Bohannon;Geol. Soc. Am. Mem.,1983

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