1887

Abstract

The evolution of evaporitic tectonic is the key in the determination of principal features of the structural model in the Bergti anticlinal belt (internal lonian subzone). The following inferences are drawn through a plentiful graphical material analysis.

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/content/papers/10.3997/2214-4609.201409736
1995-05-29
2020-06-06
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409736
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