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Abstract

Faults in brittle lithologies can form highly conductive fluid pathways at small displacements. At increasing displacement the transport properties of the fault zone are more complex. In sandstones and carbonates cataclastic gouges are formed which remain rather permeable but may be re-cemented by diagenetic fluids.

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/content/papers/10.3997/2214-4609.201405848
2003-09-08
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405848
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