1887

Abstract

Tha Adria Plate is generally considered a wide carbonate platform of principalley Mesozoic age (but started in Late Paleozoic age) covering an original African promontory. From a Triassic rifting phase, this promontory began its separation from megaplate and its northward migration and anticlockwise rotation (Finetti, 84).

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/content/papers/10.3997/2214-4609.201408430
1998-06-08
2021-06-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408430
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