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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03
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Kinematics and deformation structures in a crustal-scale shear zone on Kea (W. Cyclades, Greece)

Voit, Klaus
Grasemann, Bernhard
Draganits, Erich
Edwards, Michael A.
Müller, Monika
Iglseder, Christoph
Petrakakis, Konstantin
Exner, Ulrike
2006
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1844
Voit, Klaus; Grasemann, Bernhard; Draganits, Erich; Edwards, Michael A.; Müller, Monika; Iglseder, Christoph; Petrakakis, Konstantin; Exner, Ulrike, 2006: Kinematics and deformation structures in a crustal-scale shear zone on Kea (W. Cyclades, Greece). In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, S. 239 - 240., , DOI: 10.23689/fidgeo-1844.
 
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  • Abstract
It is generally agreed upon that the exhumation of metamorphic rocks in the Aegean is caused by post orogenic extension in the late Oligocene to early Miocene. This extension is in principle largely accommodated by low-angle crustal detachment faulting possibly resulting in the formation of metamorphic core complexes (MCC). Here, we present data from recent structural investigations on the island of Kea in the W. Cyclades, Greece. Our work focussed in the north of the island. Of the ca. 270m total structural thickness that was mapped, the entire section of rocks are highly strained. Exhumation during progressive deformation is recorded by the transition from ductile to brittle/ductile to brittle conditions. The regional characteristics and types of deformation structures vary depending on the protolith and the intensity of strain...
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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Kea
Scherzone
Deformation <Geologie>
Festlandkerne {Geologie}
Tektogenese {Geologie}
Gesteinsdeformation {Strukturgeologie}
Griechenland und griechische Inseln {Geologie}
Metamorphe Komplexe, übriges Europa {Petrologie}
Produkte mechanischer Deformation {Petrologie}
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