CHEMICAL GEOLOGY, vol.469, pp.34-46, 2017 (Peer-Reviewed Journal)
Article / Article
Science Citation Index Expanded, Scopus
Transtensional Amik Basin, Toprakkale volcanic province, Noble gases, Fluid inclusions, Trace elements, Turkey, EAST ANATOLIAN FAULT, MANTLE SOURCE, ISOTOPE SYSTEMATICS, PLATE KINEMATICS, SOUTHERN TURKEY, ORTHO-PYROXENE, KARASU VALLEY, TRACE-ELEMENT, HELIUM, SPINEL
The SE part of Turkey is characterized by a transtensional regime within the complex collision zone between the Anatolian, Arabian and African plates, which is bounded by two main faults, Dead Sea Fault and its splays on east and the Karasu Fault on west. In this tectonic and geodynamic context developed the Amik and further North, Erzin and Toprakkale districts, which are located onshore the Iskenderun Gulf, with the occurrence of a widespread and young alkaline volcanism dated from 1.57 to 0.05 Ma in Amik, and 2.25 to 0.61 Ma in Toprakkale.