@incollection{gledocs_11858_00-1735-0000-0001-3464-8,
author = {Rambousek, Christian and Grasemann, Bernhard and Petrakakis, Konstantin and Edwards, Michael A. and Iglseder, Christoph and Zámolyi, András},
editor = {Philipp, Sonja and Leiss, Bernd and Vollbrecht, Axel and Tanner, David and Gudmundsson, Agust},
title = {The Serifos Metamorphic Core Complex (Greece) — kinematic investigations of the southern detachment mylonites},
booktitle = {11. Symposium "Tektonik, Struktur- und Kristallingeologie"},
year = {2006},
publisher = {Universitätsverlag Göttingen},

abstract = {The island of Serifos is situated about 100km SSE of Athens in the Aegean Sea and belongs to the Attic-Cycladic massif. The geology of Serifos is largely characterized by a shallow hornblendebiotite granodiorite pluton that intruded in the late Miocene into a previously deformed (under blueschist conditions) sequence mainly consisting of ortho- and paragneisses, calc-silicate marbles, amphibolites and schists. The pluton has a dome-shaped body occupying the central and southern parts of the island (Salemink 1985). The Serifos MCC is the very western continuation of a zone of syn- to post tectonic intrusions younging from the East (Naxos, Paros ?12Ma) to the West (Serifos 9– 8Ma). Whereas the older intrusions in the East show a top to the North geometry, the Serifos MCC has developed a South-directed low-angle detachment fault...},
note = { \url {http://hdl.handle.net/11858/00-1735-0000-0001-3464-8}},
}