Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust-Reference-Cited by-同舟云学术

Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust

Published:1994 Issue:1-3 Volume:143 Page:425-456
ISSN:0033-4553
Container-title:Pure and Applied Geophysics PAGEOPH
language:en
Short-container-title:PAGEOPH

Author:

David Christian,Wong Teng-Fong,Zhu Wenlu,Zhang Jiaxiang

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00874337.pdf

Reference68 articles.

1. Arch, J., andMaltman, A. (1990),Anisotropic Permeability and Tortuosity in Deformed Wet Sediments, J. Geophys. Res.95, 9035?9045.

2. Bangs, N., Westbrook, G. K., Ladd, J. W., andBuhl, P. (1990),Seismic Velocities from the Barbados Ridge Complex and Indications of High Pore Pressures in an Accretionary Complex, J. Geophys. Res.95, 8767?8782.

3. Bernabé, Y. (1986),The Effective Pressure Law for Permeability in Chelmsford Granite and Barre Granite, Int. J. Rock Mech. Min. Sci and Geomech. Abst.23, 267?275.

4. Bernabé, Y. (1987),A Wide Range Permeameter for Use in Rock Physics, Int. J. Rock Mech. Min. Sci. and Geomech. Abst.24, 309?315.

5. Bernabé, Y. (1991),Pore Geometry and Pressure Dependence of the Transport Properties in Sandstones, Geophys.56, 436?446.

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