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...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | fas |
| Published: |
University of Isfahan
2019-11-01
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| Series: | Petrology |
| Subjects: | |
| Online Access: | http://ijp.ui.ac.ir/article_24088_a3b6b5d6a37a06254e9bc46ba7701891.pdf |