Late Cenozoic tectono-sedimentary evolution of the Ulukışla Basin: progressive basin development in south-central Turkey

2020 ◽  
Vol 109 (1) ◽  
pp. 345-371 ◽  
Author(s):  
Esra Gürbüz ◽  
Gürol Seyitoğlu ◽  
Ayşegül Güney
Keyword(s):  
Late Cenozoic ◽  
Sedimentary Evolution ◽  
South Central ◽  
Basin Development ◽  
Central Turkey

Elusive Complexity : New Data from late Halaf Domuztepe in South Central Turkey

Paléorient ◽  
2003 ◽  
Vol 29 (2) ◽  
pp. 117-133 ◽  
Author(s):  
Elizabeth Carter ◽  
Stuart Campbell ◽  
Suellen Gauld
Keyword(s):  
South Central ◽  
Central Turkey

Geological Correlation Between Northern Cyprus And Southern Anatolia

2021 ◽  
Author(s):  
Yucel Yilmaz
Keyword(s):  
Carbonate Platform ◽  
Middle Eocene ◽  
Source Region ◽  
Oceanic Lithosphere ◽  
Late Eocene ◽  
Central Anatolia ◽  
Late Cenozoic ◽  
Ophiolitic Mélange ◽  
South Central ◽  
Northern Cyprus

The island of Cyprus constitutes a fragment of southern Anatolia separated from the mainland by left-oblique transtension in late Cenozoic time. However, a geological framework of offset features of the south-central Anatolia, for comparison of Cyprus with a source region within and west of the southeastern Anatolian suture zone, has not yet been developed. In this paper, I enumerate, describe, and compare a full suite of potentially correlative spatial and temporal elements exposed in both regions. Northern Cyprus and south-central Anatolia have identical tectonostratigraphic units. At the base of both belts, crop out ophiolitic mélange-accretionary complex generated during the northward subduction of the NeoTethyan Oceanic lithosphere from the Late Cretaceous until the end of middle Eocene. The nappes of the Taurus carbonate platform were thrust above this internally chaotic unit during late Eocene. They began to move as a coherent nappe pile from that time onward. An asymmetrical flysch basin was formed in front of this southward moving nappe pile during the early Miocene. The nappes were then thrust over the flysch basin fill and caused its tight folding. Cyprus separated from Anatolia in the Pleistocene-Holocene when, transtensional oblique faults with dip-slip components caused the development of the Adana and Iskenderun basins and the separation of Cyprus from Anatolia.

Late Cenozoic calc-alkaline volcanism over the Payenia shallow subduction zone, South-Central Andean back-arc (34°30′–37°S), Argentina

2015 ◽  
Vol 64 ◽  
pp. 365-380 ◽  
Author(s):  
Vanesa D. Litvak ◽  
Mauro G. Spagnuolo ◽  
Andrés Folguera ◽  
Stella Poma ◽  
Rosemary E. Jones ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Late Cenozoic ◽  
Calc Alkaline ◽  
South Central ◽  
Alkaline Volcanism ◽  
Shallow Subduction ◽  
Back Arc

scholarly journals Evaluation of prenatally diagnosed fetal sacrococcygeal teratomas: A case series of seventeen pregnancies from South-central Turkey

2020 ◽  
Vol 17 (3) ◽  
pp. 170-174
Author(s):  
Mehmet Özsürmeli ◽  
Selim Büyükkurt ◽  
Mete Sucu ◽  
Erol Arslan ◽  
Selahattin Mısırlıoğlu ◽  
...  
Keyword(s):  
Case Series ◽  
South Central ◽  
Central Turkey
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