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Abstract

Formation of a Late Cretaceous thrust and fold belt was followed by major wrench faulting which eventually juxtaposed the originally distant orogenic terranes making up now the substrata of the Pannonian basin.

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/content/papers/10.3997/2214-4609.201410211
1994-06-10
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410211
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