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Abstract

Details of the sea floor and of deformational styles of large portions of the central and eastern Mediterranean Ridge (MR) are revealed in recent 100% coverage swath bathymetry, acoustic imagery, together with continuons seismic profiling.The MR is a wide accretionnary wedge that results from convergente and ongoing incipient collision between Europe, Africa and the Anatolia-Aegea microplate, in Eastern Mediterranean.

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/content/papers/10.3997/2214-4609.201406008
2000-10-01
2021-07-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406008
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