From oceanic to continental subduction: Implications for the geochemical and redox evolution of the supra-subduction mantle
نویسندگان
چکیده
منابع مشابه
Role of supra-subduction zone ophiolites in the tectonic evolution of the southeastern Zagros Orogenic Belt, Iran
Ophiolitic rocks in the southeastern part of the Zagros Orogenic Belt can be separated from southwest to northeast, into two groups: the Neyriz ophiolites and the Naien–Shahrebabak–Baft ophiolites. The southeast sector of Sanandaj-Sirjan wasdelimited by the two nearly synchronous ophiolitic belts in its southwestern and northeastern margins. In this study, new ophiolitic formation models were u...
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ژورنال
عنوان ژورنال: Geosphere
سال: 2018
ISSN: 1553-040X
DOI: 10.1130/ges01597.1