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Abstract

Clay smear is an important process in siliciclastic sequences, but the details of the evolution of fault zones in sand-clay layered sequences are poorly understood. This project presents the results of an experimental investigation of clay smear processes, using a geotechnical direct shear apparatus.

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/content/papers/10.3997/2214-4609.201405849
2003-09-08
2024-04-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405849
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