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Abstract

Although salt structures can assume complex geometries, their gross regional distribution in a salt province is often observed to follow a more simple and regular pattern that can be mathematically described in terms of an initial horizontal salt flow caused by loading variations in the overburden.

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/content/papers/10.3997/2214-4609.201405989
2000-10-01
2021-08-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405989
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