Mineral chemistry of high-Al chromian spinel from ultramafic rocks of the Babina–Prithvipur transect, Bundelkhand Craton, central India: Implication for petrogenesis and tectonic setting-Reference-Cited by-同舟云学术

Mineral chemistry of high-Al chromian spinel from ultramafic rocks of the Babina–Prithvipur transect, Bundelkhand Craton, central India: Implication for petrogenesis and tectonic setting

Published:2020-08-31 Issue:1 Volume:129 Page:
ISSN:2347-4327
Container-title:Journal of Earth System Science
language:en
Short-container-title:J Earth Syst Sci

Author:

Sahu Abinash,Vishwakarma Neeraj^ORCID,Singh Yamuna,Verma C B

Funder

National Institute of Technology Raipur

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s12040-020-01448-3.pdf

Reference87 articles.

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3. Ahmed A H, Arai S and Attia A K 2001 Petrological characteristics of podiform chromitites and associated peridotites of the Pan African proterozoic ophiolite complexes of Egypt; Miner. Deposita 36 72–84.

4. Allan J F, Sack R O and Batiza R 1988 Cr-rich spinels as petrogenetic indicators; MORB-type lavas from the Lamont seamount chain, Eastern Pacific; Am. Miner. 73(7–8) 741–753.

5. Arai S 1987 An estimation of the least depleted spinel peridotite on the basis of olivine-spinel mantle array; N. Jb. Miner. Mh. 8 347–354.

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