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Abstract

In convergent margins, tectonic wedges (especially thick - accretionary prisms) are frequently affected by shale diapirism and mud extrusion processes which influence both the structural evolution and the fluid dynamics within the tectonic wedge.

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/content/papers/10.3997/2214-4609.201406081
2000-10-01
2024-04-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406081
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