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Abstract

The western Prerif area, located in northem Morocco, constitutes the most extemal structural unit of the Rif Alpine domain which inciudes essentially Mesozoic and Cenozoic folded sediment overlaying the Paleozoic basement.

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/content/papers/10.3997/2214-4609.201406015
2000-10-01
2021-09-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406015
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