Evidence of melt– and fluid–rock interactions in the refractory forearc peridotites and associated mafic intrusives from the Tuting–Tidding ophiolites, eastern Himalaya, India: Petrogenetic and tectonic implications-Reference-Cited by-同舟云学术

Evidence of melt– and fluid–rock interactions in the refractory forearc peridotites and associated mafic intrusives from the Tuting–Tidding ophiolites, eastern Himalaya, India: Petrogenetic and tectonic implications

Published:2020-11-23 Issue:4 Volume:56 Page:2082-2110
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Dutt Amrita¹^ORCID,Singh Athokpam Krishnakanta¹^ORCID,Srivastava Rajesh K.²^ORCID,Oinam Govind¹^ORCID

Affiliation:

1. Petrology & Geochemistry Group Wadia Institute of Himalayan Geology Dehradun India

2. Department of Geology Banaras Hindu University Varanasi India

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4043

Reference160 articles.

1. The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both?

2. Heterogeneously depleted Precambrian lithosphere deduced from mantle peridotites and associated chromitite deposits of Al'Ays ophiolite, Northwestern Arabian Shield, Saudi Arabia

3. Detrital zircon U–Pb ages along the Yarlung-Tsangpo suture zone, Tibet: Implications for oblique convergence and collision between India and Asia

4. Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry

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