Permeability and seismic velocity anisotropy across a ductile–brittle fault zone in crystalline rock

This study characterizes the elastic and fluid flow properties systematically across a ductile–brittle fault zone in crystalline rock at the Grimsel Test Site underground research laboratory. Anisotropic seismic velocities and permeability measured every 0.1 m in the 0.7 m across the transition z...

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Bibliographic Details
Main Authors: Q. C. Wenning, C. Madonna, A. de Haller, J.-P. Burg
Format: Article
Language:English
Published: Copernicus Publications 2018-05-01
Series:Solid Earth
Online Access:https://www.solid-earth.net/9/683/2018/se-9-683-2018.pdf