Low hydrogen concentrations in Dharwar cratonic lithosphere inferred from peridotites, Wajrakarur kimberlites field: Implications for mantle viscosity and carbonated silicate melt metasomatism-Reference-Cited by-同舟云学术

Low hydrogen concentrations in Dharwar cratonic lithosphere inferred from peridotites, Wajrakarur kimberlites field: Implications for mantle viscosity and carbonated silicate melt metasomatism

Published:2021-01 Issue: Volume:352 Page:105982
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Pattnaik Jiten,Demouchy Sylvie,Ghosh Sujoy

Funder

Science and Engineering Research Board

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference163 articles.

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1. Recent Studies on Volcanic Materials and Chemistry of the Earth’s Interior - An Indian Perspective;Journal of the Geological Society of India;2024-02-01

2. Origin of clinopyroxene megacrysts from the 1.1 Ga Chigicherla-4 kimberlite (CC4), Dharwar craton, southern India: Implications for multi-stage metasomatism of the sub-continental lithospheric mantle;Journal of Asian Earth Sciences;2023-04

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4. Major and trace element geochemistry of olivine from an ENE-trending picrite dyke, genetically linked to the ca. 1.89–1.88 Ga Hampi swarm, western Dharwar craton: Implications for plume induced melting of a mixed peridotite-pyroxenite source;Geochemistry;2021-11