Forearc lava stratigraphy of the Beila Ophiolite, north-central Tibetan Plateau: Magmatic response to initiation of subduction of the Bangong-Nujiang Meso-Tethys Ocean-Reference-Cited by-同舟云学术

Forearc lava stratigraphy of the Beila Ophiolite, north-central Tibetan Plateau: Magmatic response to initiation of subduction of the Bangong-Nujiang Meso-Tethys Ocean

Published:2021-11 Issue: Volume:582 Page:110663
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Tang Yue,Zhai Qing-Guo,Hu Pei-Yuan,Wang Wei,Yan Zhen,Wang Hai-Tao,Zhu Zhi-Cai

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of the People's Republic of China

China Postdoctoral Science Foundation

China Geological Survey

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference113 articles.

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4. Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: constraints on the trace element chemistry of mantle and deep crustal fluids;Brenan;Geochim. Cosmochim. Acta,1995

5. Petrology and origin of primitive lavas from the Troodos ophiolite, Cyprus;Cameron;Contrib. Mineral. Petrol.,1985

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