Mineral chemistry and termometry of the high-Mg ultramafic lava flows (Komatiite), NE Iran: evidence of plume-arc interaction in the Upper Paleozoic Mashhad-Fariman subduction zone

In the northeast of Iran, there are some outcrops of high-Mg ultramafic volcanic rocks. These rocks have been interpreted as an ideal ophiolite sequence related to the closure of Paleo-Tethys. According to detailed field observations, the komatiitic lava flows in Shandiz- Virani- Mashhad Complex (SV...

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Bibliographic Details

Published in:	پترولوژی
Main Authors:	Mohsen Mobasheri, Habibollah Ghasemi, Behnam Rahimi, Arash Gourabjiri-pour
Format:	Article
Language:	Persian
Published:	University of Isfahan 2019-11-01
Subjects:	mineral chemistry thermometry komatiite mashhad fariman iran
Online Access:	http://ijp.ui.ac.ir/article_24088_a3b6b5d6a37a06254e9bc46ba7701891.pdf