Origin of Indus ophiolite-hosted ophicarbonate veins: Isotopic evidence of mixing between seawater and continental crust-derived fluid during Neo-Tethys closure-Reference-Cited by-同舟云学术

Origin of Indus ophiolite-hosted ophicarbonate veins: Isotopic evidence of mixing between seawater and continental crust-derived fluid during Neo-Tethys closure

Published:2020-09 Issue: Volume:551 Page:119772
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Das Souvik^ORCID,Basu Asish R.,Mukherjee Barun K.,Marcantonio Franco,Sen Koushick,Bhattacharya Satadru,Gregory Robert T.

Funder

University of Texas

Wadia Institute of Himalayan Geology

Southern Methodist University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference44 articles.

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3. The relationship between fluids in some fresh alpine-type ultramafics and possible modern serpentinization, western United States;Barnes;Geol. Soc. Am. Bull.,1969

4. Mantle upwelling from ~410 km transition zone below the Neo-Tethyan Indus ophiolite in Nidar, NW Himalaya;Basu,2016

5. Ultramafic carbonate breccias from the equatorial Mid-Atlantic Ridge;Bonatti;Mar. Geol.,1974

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