Atıf İçin Kopyala
Italiano F., YÜCE G., Di Bella M., Rojay B., Sabatino G., Tripodo A., ...Daha Fazla
CHEMICAL GEOLOGY, cilt.469, ss.34-46, 2017 (SCI-Expanded)
-
Yayın Türü:
Makale / Tam Makale
-
Cilt numarası:
469
-
Basım Tarihi:
2017
-
Doi Numarası:
10.1016/j.chemgeo.2017.04.003
-
Dergi Adı:
CHEMICAL GEOLOGY
-
Derginin Tarandığı İndeksler:
Science Citation Index Expanded (SCI-EXPANDED), Scopus
-
Sayfa Sayıları:
ss.34-46
-
Anahtar Kelimeler:
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
-
Orta Doğu Teknik Üniversitesi Adresli:
Evet
Özet
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.