1887

Abstract

A kinematic model describing fault-bend folding combined with a diffusion model simulating sedimentation and erosion is used to investigate the effects of fault geometry, changes in displacement-rate and sequence of fault activation on contemporaneous sedimentation.

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/content/papers/10.3997/2214-4609.201408947
1996-06-04
2020-08-13
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408947
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