Lithospheric boudinage in the Western Me
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E. Gueguen; C. Doglioni; M. Fernandez
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Article
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1997
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John Wiley and Sons
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English
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The western Mediterranean is composed of irregular troughs formed as backβarc basins in the hanging wall of the Wβdirected Apenninic subduction which retreated eastward during Neogene and Quaternary times. The basins are progressively younger toward the east, ageing from late Oligoceneβearly Miocene