• Medientyp: E-Artikel
  • Titel: The Serifos Metamorphic Core Complex (Greece) — kinematic investigations of the southern detachment mylonites
  • Beteiligte: Rambousek, Christian [VerfasserIn]; Grasemann, Bernhard [VerfasserIn]; Petrakakis, Konstantin [VerfasserIn]; Edwards, Michael A. [VerfasserIn]; Iglseder, Christoph [VerfasserIn]; Zámolyi, András [VerfasserIn]; Philipp, Sonja [VerfasserIn]; Leiss, Bernd [VerfasserIn]; Vollbrecht, Axel [VerfasserIn]; Tanner, David [VerfasserIn]; Gudmundsson, Agust [VerfasserIn]
  • Erschienen: Universitätsverlag Göttingen, 2006
  • Sprache: Deutsch
  • DOI: https://doi.org/10.23689/fidgeo-1917
  • Schlagwörter: Serifos ; Scherzone ; Krustenbewegung ; Mylonit
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  • Beschreibung: 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. ; conference
  • Zugangsstatus: Freier Zugang