THE EMPLACEMENT OF THE VERMION NAPPE IN THE AREA OF KATO SELI (MT VERMION, CENTRAL MACEDONIA, GREECE) | Zendy

George Georgiadis | Zendy; Μάρκος Δ. Τρανός | Zendy; Αδαμάντιος Κίλιας | Zendy; D. Mountrakis | Zendy

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THE EMPLACEMENT OF THE VERMION NAPPE IN THE AREA OF KATO SELI (MT VERMION, CENTRAL MACEDONIA, GREECE)

Author(s) -

George Georgiadis,

Μάρκος Δ. Τρανός,

Αδαμάντιος Κίλιας,

D. Mountrakis

Publication year - 2017

Publication title -

bulletin of the geological society of greece

Language(s) - English

Resource type - Journals

eISSN - 2529-1718

pISSN - 0438-9557

DOI - 10.12681/bgsg.11698

Subject(s) - nappe , flysch , geology , tectonics , paleontology , geochemistry

Our fieldwork in the area of Kato Seli of Mt Vermion suggests that the Vermion Nappe is not only tectonically overlying the Maastrichtian flysch of the Pelagonian Zone, but also a Jurassic melange that overlies the Triassic-Jurassic marbles of the Pelagonian Zone. Moreover, between the Vermion Nappe and the underlying melange, tectonic slivers of meta-sandstones-meta-rudites are tectonically emplaced. This calls for a reassessment of the emplacement of the Vermion Nappe and its role in the geotectonic evolution of the area.

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