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Comment on 'Rockfall avalance deposits associated with normal faulting in the NW of the Cankiri basin: implications for the post-collisional tectonic evolution of the Neo-Tethyan suture zone' by G. Seyitoglu, N. Kazanci, L. Karadenizli, S. Sen, B. Varol, and T. Karabiyikoglu
Date
2003-04-01
Author
Kaymakcı, Nuretdin
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Seyitoglu et al. (2000) described their interpretation, based on a single fault surface and rockfall avalanche deposits previously mapped as a W-vergent thrust klippen above the Neogene successions in the Hancili Basin, that in central Anatolia there was a single extensional basin throughout the Miocene - Early Pliocene. It was later fragmented by a structural high of Neo-Tethyan ophiolitic basement bounded by an E-vergent thrust fault in the east along the western margin of the Cankiri Basin and a west-dipping normal fault in the west along the eastern margin of the Hancili Basin, into two sub-basins - Cankiri and Hancili basins - subsequent to the activity along the Kirikkale-Erbaa splay of the North Anatolian Fault Zone in the Late Pliocene (Fig. 1b). They also concluded that the crustal extension commenced in the Early Miocene and continued until the Early Pliocene without a break. They further claimed that their contention is supported by the recent works of Kaymakci (2000) and Kaymakciet al. (2000).
Subject Keywords
Geology
URI
https://hdl.handle.net/11511/48719
Journal
TERRA NOVA
DOI
https://doi.org/10.1046/j.1365-3121.2003.00468.x
Collections
Department of Geological Engineering, Article
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N. Kaymakcı, “Comment on ‘Rockfall avalance deposits associated with normal faulting in the NW of the Cankiri basin: implications for the post-collisional tectonic evolution of the Neo-Tethyan suture zone’ by G. Seyitoglu, N. Kazanci, L. Karadenizli, S. Sen, B. Varol, and T. Karabiyikoglu,”
TERRA NOVA
, pp. 133–136, 2003, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/48719.