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Abstract

The Mediterranean region is populated by two sets of orogenic systems: (1) those that<br>are made up of topographically high mountains that appear to have directly accommodated<br>the continuing convergence of Africa and Eurasia, and (2) those that are made up of<br>topographically low mountains that do not accommodate Africa-Eurasia convergence directly.<br>The latter are characterized by regional-scale extension within the upper plate and typically<br>propagate at high angles to the direction of Europe-Africa convergence.

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/content/papers/10.3997/2214-4609.201405739
2002-05-27
2022-12-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405739
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