MANTLE UPWELLING FROM ~ 410 KM TRANSITION ZONE BELOW THE NEO - TETHYAN INDUS OPHIOLITE IN NIDAR, NW HIMALAYA. BASU,
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Geological Society of America
Cited by 2 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. The Indian Ocean, its supra-subduction history, and implications for ophiolites;Plate Tectonics, Ophiolites, and Societal Significance of Geology: A Celebration of the Career of Eldridge Moores;2021-09-09
2. Origin of Indus ophiolite-hosted ophicarbonate veins: Isotopic evidence of mixing between seawater and continental crust-derived fluid during Neo-Tethys closure;Chemical Geology;2020-09
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