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Evolution of the Adria-Europe plate boundary in the northern Dinarides: From continent-continent collision to back-arc extension

TECTONICS, no. 6 (2010)

Cited by: 73|Views8
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Abstract

The Sava Zone of the northern Dinarides is part of the Cenozoic Adria-Europe plate boundary. Here Late Cretaceous subduction of remnants of Meliata-Vardar oceanic lithosphere led to the formation of a suture, across which upper plate European-derived units of Tisza-Dacia were juxtaposed with Adria-derived units of the Dinarides. Late Cret...More

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