1887

Abstract

Faults are frequently segmented both in map view and in cross-section. Displacement is transferred between adjacent fault segments with high displacement gradients via a zone of high strain, often referred to as a relay zone.

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/content/papers/10.3997/2214-4609.201405844
2003-09-08
2020-09-22
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405844
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