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Geodynamic evolution of the Adriatic-Dinaric carbonate platform.

The Adria or apulian plate initiated rifting during the Middle Triassic. During the Early Jurassic, due to extensional block-faulting in the south Tethyan realm, the Adriat. -Dinar. carbonate platform (ADACP) was individualized as one among the numerous carbonate platform settings, separated by deep-water throughts with pelagic sedimentation.

Adriatic-Dinaric carbonate platform; geodynamic evolution

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