Origin and evolution of Suru Valley ophiolite peridotite slice along Indus suture zone, Ladakh Himalaya, India: Implications on melt-rock interaction in a subduction-zone environment-Reference-Cited by-同舟云学术

Origin and evolution of Suru Valley ophiolite peridotite slice along Indus suture zone, Ladakh Himalaya, India: Implications on melt-rock interaction in a subduction-zone environment

Published:2019-04 Issue:1 Volume:79 Page:78-93
ISSN:0009-2819
Container-title:Geochemistry
language:en
Short-container-title:Geochemistry

Author:

Bhat Irfan Maqbool,Ahmad Talat,Subba Rao D.V.

Funder

Council of Scientific and Industrial Research (CSIR)

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference133 articles.

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3. Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry;Arai;Mineral. Mag.,1992

4. Compositional variation of olivine-chromian spinel in Mg-rich magma as a guide to their residual spinel peridotites;Arai;J. Volcanol. Geotherm. Res.,1994

5. Podiform chromitites do form beneath mid-ocean ridges;Arai;Lithos,2015

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