Refertilization of depleted mantle peridotite in the <scp>Nagaland–Manipur</scp> ophiolite, north‐east India: Constraints from <scp>PGE</scp> , mineral, and whole‐rock geochemistry-Reference-Cited by-同舟云学术

Refertilization of depleted mantle peridotite in the Nagaland–Manipur ophiolite, north‐east India: Constraints from PGE , mineral, and whole‐rock geochemistry

Published:2022-03-15 Issue:12 Volume:57 Page:5265-5283
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Chaubey Monika¹^ORCID,Singh Athokpam Krishnakanta¹,Singh Birendra P.²,Imtisunep Sashimeren¹^ORCID,Dutt Amrita¹^ORCID,Satyanarayanan Manavalan³^ORCID,Premi Kshetrimayum⁴,Abhirami Sethuraman G.³

Affiliation:

1. Wadia Institute of Himalayan Geology Dehradun India

2. Department of Geology Banaras Hindu University Varanasi India

3. National Geophysical Research Institute Hyderabad India

4. Department of Geology Indian Institute of Technology Roorkee India

Funder

Ministry of Earth Sciences

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4411

Reference107 articles.

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3. Agrawal O. P.&Ghose N. C.(1986).Geology and stratigraphy of the Naga Hills ophiolite between Melluri and Awankhoo Pheek District Nagaland India. InIndian chapter IGCP Projects195 and 197. Meeting 63–195.

4. Tectonic Evolution of the Western Margin of the Burma Microplate Based on New Fossil and Radiometric Age Constraints

5. Mid-ocean ridge and supra-subduction geochemical signatures in spinel–peridotites from the Neotethyan ophiolites in SW Turkey: Implications for upper mantle melting processes

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