1887

Abstract

Detailed structural - geological research was carried out around the Sudetic Marginal Fault, the most important tectonic structure in the NE part of the Bohemian Massif. The fault divides methamophic rocks like crystalline limestones, gneisses and schists

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/content/papers/10.3997/2214-4609.201400023
2009-06-08
2021-10-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400023
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