Authigenic carbonate mineral formation in the Pagassitikos palaeolake during the latest Pleistocene, central Greece

Authigenic carbonate mineral formation in the Pagassitikos palaeolake during the latest Pleistocene, central Greece

The Pagassitikos Gulf in Greece is a semi-enclosed bay with a maximum depth of 102 m. According to the present-day bathymetric configuration and the sea level during the latest Pleistocene, the gulf would have been isolated from the open sea, forming a palaeolake since ~32 cal. ka b. p. Sediment cor...

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Bibliographic Details
Main Author: Hallberg, Rolf O. (author)
Other Authors: Kanellopoulos, Theodore D. (author), Koutsopoulou, Eleni (author), Kosmas Pavlopoulos (author), Schmidt, Mark (author), Karageorgis, Aristomenis P. (author), Tripsanas, Efthymios K. (author), Anagnostou, Christos L. (author), Mavromatis, Vasileios (author)
Published: 2012
Online Access:http://hdl.handle.net/20.500.12458/313
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http://hdl.handle.net/20.500.12458/313

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