Miocene south directed low-angle normal fault evolution on Kea Island (West Cycladic Detachment System, Greece)
Author:
Affiliation:
1. Department for Geodynamics and Sedimentology; University of Vienna; Vienna; Austria
2. Department of Earth Sciences; University of Ottawa; Ottawa, Ontario; Canada
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/tc/tc1104/2010TC002802/2010TC002802.pdf
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3. A late Oligocene/early Miocene high temperature belt in the Attic-Cycladic crystalline complex (SE Pelagonian, Greece);Altherr;Geol. Jahrb.,1982
4. O-Sr isotopic variations in Miocene granitoids from the Aegean: Evidence for an origin by combined assimilation and fractional crystallization;Altherr;Contrib. Mineral. Petrol.,1988
5. Dating the events of metamorphism and granitic magmatism in the Alpine orogen of Naxos (Cyclades, Greece);Andriessen;Contrib. Mineral. Petrol.,1979
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