The Arkot Dağ Melange, Central Turkey: Evidence for the geodynamic evolution of the Intra-Pontide Suture Zone.

Date

2014-09-24

Author

Pandolfi, L.
Göncüoğlu, Mehmet Cemal
Marroni, M.
Ellero, A.
Ottria, G.
Catanzariti, R.
Tekin, Uğur Kağan
Sayıt, Kaan

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https://hdl.handle.net/11511/98068

Conference Name

XX. Congress of the Carpathian Balkan Geological Association

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Department of Geological Engineering, Conference / Seminar

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The Arkotdag Melange, Central Turkey: Evidence for the Geodynamic Evolution of the Intra-Pontide Suture Zone Pandolfi, L.; Göncüoğlu, Mehmet Cemal; Marroni, M.; Ellero, A.; Ottria, G.; Catanzariti, R.; Tekin, Uğur Kağan; Sayıt, Kaan (2014-12-08)
The Arkot Dag Melange in Arac area, central Turkey: Evidence of its origin within the geodynamic evolution of the Intra-Pontide suture zone Goncuoglu, M. Cemal; Marroni, Michele; Pandolfi, Luca; Eller, Alessandro; Ottria, Giuseppe; Catanzariti, Rita; TEKİN, UĞUR KAĞAN; Sayıt, Kaan (Elsevier BV, 2014-05-01) In northern Turkey, the Intra-Pontide suture zone is represented by an east-west trending belt of deformed and/or metamorphic units located at the boundary between the Istanbul-Zonguldak terrane to the north and the Sakarya terrane to the south. These units can be regarded as issued from the Intra-Pontide domain, whose geodynamic history is still a matter of debate. Along the Akpinar-Arac-Bayramoren geotraverse, located in central Turkey, an ophiolite-bearing melange known as the Arkot Dag Melange, is well-...
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Citation Formats

L. Pandolfi et al., “The Arkot Dağ Melange, Central Turkey: Evidence for the geodynamic evolution of the Intra-Pontide Suture Zone.,” presented at the XX. Congress of the Carpathian Balkan Geological Association, Tirane, Arnavutluk, 2014, Accessed: 00, 2022. [Online]. Available: https://hdl.handle.net/11511/98068.