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BECCALETTO, LAURENT, BONEV, NIKOLAY, BOSCH, DELPHINE, BRUGUIER, OLIVIER (2007) Record of a Palaeogene syn-collisional extension in the north Aegean region: evidence from the Kemer micaschists (NW Turkey) Geological Magazine, 144 (2) 393-400 doi:10.1017/s001675680700310x

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Reference TypeJournal (article/letter/editorial)
TitleRecord of a Palaeogene syn-collisional extension in the north Aegean region: evidence from the Kemer micaschists (NW Turkey)
JournalGeological Magazine
AuthorsBECCALETTO, LAURENTAuthor
BONEV, NIKOLAYAuthor
BOSCH, DELPHINEAuthor
BRUGUIER, OLIVIERAuthor
Year2007 (March)Volume144
Issue2
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s001675680700310xSearch in ResearchGate
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Mindat Ref. ID260026Long-form Identifiermindat:1:5:260026:4
GUID0
Full ReferenceBECCALETTO, LAURENT, BONEV, NIKOLAY, BOSCH, DELPHINE, BRUGUIER, OLIVIER (2007) Record of a Palaeogene syn-collisional extension in the north Aegean region: evidence from the Kemer micaschists (NW Turkey) Geological Magazine, 144 (2) 393-400 doi:10.1017/s001675680700310x
Plain TextBECCALETTO, LAURENT, BONEV, NIKOLAY, BOSCH, DELPHINE, BRUGUIER, OLIVIER (2007) Record of a Palaeogene syn-collisional extension in the north Aegean region: evidence from the Kemer micaschists (NW Turkey) Geological Magazine, 144 (2) 393-400 doi:10.1017/s001675680700310x
In(2007, March) Geological Magazine Vol. 144 (2) Cambridge University Press (CUP)
Abstract/NotesIn NW Turkey, the medium-grade Kemer micaschists of the Biga Peninsula record NE-directed extension related to ductile to brittle–ductile shearing during the Palaeogene period: a lower limit for their exhumation is given by the Late Maastrichtian age of the HP–LT metamorphism of a similar nearby area (Çamlıca micaschists); an upper limit is given by the Early Eocene intrusion age of the post-kinematic Karabiga granitoid, dated as 52.7 ± 1.9 Ma using the U–Pb LA–ICP–MS method on xenotime. Correlations with the northeasterly Rhodope region and integration into the geodynamic regional frame indicate that the Kemer micaschists experienced an extensional deformation connected to a collisional context in latest Cretaceous–early Tertiary times. The Kemer micaschists therefore represent a new area (the first in Turkey), which suffered synorogenic extension in the north Aegean domain at the very beginning of Tertiary times.


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