Compositional signatures of clinopyroxenes from the mafic rocks of the Nagaland ophiolite (NE India): Inferences for melting of diverse source regions in a transitional arc-type setting-Reference-Cited by-同舟云学术

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Compositional signatures of clinopyroxenes from the mafic rocks of the Nagaland ophiolite (NE India): Inferences for melting of diverse source regions in a transitional arc-type setting

Published:2024-06 Issue: Volume: Page:126150
ISSN:0009-2819
Container-title:Geochemistry
language:en
Short-container-title:Geochemistry

Author:

Wangjam Monica,Maibam Bidyananda,Foley Stephen,Kapsiotis Argyrios

Funder

Council of Scientific and Industrial Research, India

Department of Science and Technology

Publisher

Elsevier BV

Reference101 articles.

1. Indo-Burma Range: a belt of accreted microcontinents, ophiolites and Mesozoic–Paleogene flyschoid sediments;Acharyya;Int. J. Earth Sci.,2015

2. Tectono-stratigraphy and emplacement history of the ophiolite assemblage from the Naga Hills and Andaman island-arc, India;Acharyya;J. Geol. Soc. India,1989

3. Geology of Nagaland ophiolite;Anon;Mem. Geol. Surv. India,1986

4. Clinopyroxenes from alkaline rocks of Japan;Aoki;Am. Mineral.,1964

5. Relationship between clinopyroxene composition and the formation environment of volcanic host rocks;Aparicio;IUP J. Earth Sci.,2010

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