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The Memory of a Fault Gouge: An Example from the Simplon Fault Zone (Central Alps)

Faut gouge forms at the core of the fault as the result of a slip in the upper brittle crust. Therefore, the deformation mechanisms and conditions under which the fault gouge was formed can document the stages of fault movement in the crust. We carried out a microstructural analysis on a fault gouge...

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主要な著者: Valentina Argante, David Colin Tanner, Christian Brandes, Christoph von Hagke, Sumiko Tsukamoto
フォーマット: Artigo
言語:Inglês
出版事項: MDPI AG 2022-06-01
シリーズ:Geosciences
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オンライン・アクセス:https://www.mdpi.com/2076-3263/12/7/268
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