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The Serifos Metamorphic Core Complex (Greece) — kinematic investigations of the southern detachment mylonites

Rambousek, Christian
Grasemann, Bernhard
Petrakakis, Konstantin
Edwards, Michael A.
Iglseder, Christoph
Zámolyi, András
2006
Universitätsverlag Göttingen
Article in Anthology
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Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1917
In: 11. Symposium "Tektonik, Struktur- und Kristallingeologie"
Rambousek, Christian; Grasemann, Bernhard; Petrakakis, Konstantin; Edwards, Michael A.; Iglseder, Christoph; Zámolyi, András, 2006: The Serifos Metamorphic Core Complex (Greece) — kinematic investigations of the southern detachment mylonites. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Universitätsverlag Göttingen, p. 172-173, DOI 10.23689/fidgeo-1917.
 
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  • 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...
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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Serifos
Scherzone
Mylonit
Krustenbewegung
Griechenland und griechische Inseln {Geologie}
Metamorphe Komplexe, übriges Europa {Petrologie}
Produkte mechanischer Deformation {Petrologie}
Gesteinsdeformation {Strukturgeologie}
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