Footwall mineralization during Late Miocene extension along the West Cycladic Detachment System, Lavrion, Greece

Author:

Berger Alexandra1,Schneider David A.1,Grasemann Bernhard2,Stockli Daniel3

Affiliation:

1. Department of Earth Sciences; University of Ottawa; Ottawa; ON; K1N 6N5; Canada

2. Department of Geodynamics and Sedimentology; University of Vienna; A-1090; Vienna; Austria

3. Department of Geological Sciences; University of Texas; Austin; TX; 78712; USA

Publisher

Wiley

Subject

Geology

Reference38 articles.

1. I-type plutonism in a continental back-arc setting: Miocene granitoids and monzonites from the central Aegean Sea, Greece;Altherr;Contrib. Mineral. Petrol.,2002

2. A late Oligocene/early Miocene high temperature belt in the Attic-Cycladic crystalline complex (SE Pelagonian, Greece);Altherr;Geol. Jb.,1982

3. Back arc extension and denudation of Mediterranean eclogites;Avigad;Tectonics,1997

4. Block rotations and continental extension in the central Aegean Sea: palaeomagnetic and structural evidence from Tinos and Mykonos (Cyclades, Greece);Avigad;Earth Planet. Sci. Lett.,1998

5. Contact metamorphism of calc-silicate hornfels from Plaka area, Lavrium, Greece;Baltatzis;N. Jb. Miner. Mh.,1981

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