1887

Abstract

In this paper we consider the controls on the fabric of mudstones on scales ranging from 10 microns to 100 metres, and how this might affect fluid flow regimes within mud-rich caprock sequences.

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/content/papers/10.3997/2214-4609.201405869
2003-09-08
2021-06-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405869
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