1887

Abstract

A general statement relate fracturing to tectonic events. In carbonates, the strong influence of diagenetic processes through time is a clue in rock brittle properties acquisition. Indeed,in such host-rock, early cementation developed rapidly after deposition and turn the deposited sediment into a brittle rock, allowing fracture to develop through burial. What we want to show is how these mechanism have to be taken into account when characterizing the fracture pattern in carbonates.

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/content/papers/10.3997/2214-4609.20132002
2013-12-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20132002
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