Mesozoic/Cenozoic sedimentation and tectonics of the southern Greek Neotethys (Argolis peninsula)
The Argolis Peninsula of SE Greece lies within the Alpine orogenic belt, which formed as a result of continental collision, following the closure of a Mesozoic-Tertiary Neotethys oceanic basin. The area is located at the southern end of the Pelagonian Zone, a microcontinental block, which rifted fro...
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University of Edinburgh
1990
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.643268 |