1887

Abstract

The Apenninic-Maghrebian Orogen comprises the whole oroclinalic bell which originated from North Africa to Central Italy, during the Neogene Africa-Europe collision. It represents the dominant structural domain of the Central Mediterranean region, as it is located between the Sardinian Block, a European fragment, and the margins of the Adria and African plates. These latter, together with the oceanic Ionian Basin located between them, act as foreland areas.

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/content/papers/10.3997/2214-4609.201409611
1995-05-29
2021-05-07
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409611
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