Synchrotron 3D microtomography of halite aggregates during experimental pressure solution creep and evolution of the permeability-Reference-Cited by-同舟云学术

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Synchrotron 3D microtomography of halite aggregates during experimental pressure solution creep and evolution of the permeability

Published:2004-04-03 Issue:7 Volume:31 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Renard François¹²,Bernard Dominique³,Thibault Xavier⁴,Boller Elodie⁴

Affiliation:

1. Laboratoire de Géophysique Interne et Tectonophysique; Université Joseph Fourier; Grenoble France

2. Physics of Geological Processes; University of Oslo; Oslo Norway

3. Institut de Chimie de la Matière Condensée de Bordeaux; Pessac France

4. European Synchrotron Radiation Facility; Grenoble France

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference18 articles.

1. The local change of scale method for modeling flow in natural porous media (I): Numerical tools;Anguy;Adv. Water Resour.,1994

2. Using the Volume Averaging Technique to Perform the First Change of Scale for Natural Random Porous Media

3. Universal scaling in transient creep;Dysthe;Phys. Rev. Lett.,2002

4. Modelling fluid transfer along Californian faults when integrating pressure solution crack-sealing and compaction processes;Gratier;J. Geophys. Res.,2003

5. Stylolites in sandstones;Heald;Geology. J.,1955

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