Pyroxenite–harzburgite sequences in the Dazhuqu ophiolite (Southern Tibet) formed through hydrous melt infiltration and melt–peridotite reaction-Reference-Cited by-同舟云学术

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Pyroxenite–harzburgite sequences in the Dazhuqu ophiolite (Southern Tibet) formed through hydrous melt infiltration and melt–peridotite reaction

Published:2023-11-22 Issue:12 Volume:178 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Zhang Zhen-Yu,Liu Chuan-Zhou,Liang Yan,Liu Tong,Zhang Chang,Liu Bo-Da,Lin Yin-Zheng,Zhang Wei-Qi,Ji Wen-Bin

Funder

National Science Fund for Distinguished Young Scholars

National Key Research and Development Project of China

National Science Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00410-023-02076-y.pdf

Reference142 articles.

1. Abrajevitch A, Ali J, Aitchison J, Badengzhu DA, Liu J, Ziabrev S (2005) Neotethys and the India-Asia collision: Insights from a palaeomagnetic study of the Dazhuqu ophiolite, southern Tibet. Earth Planet Sci Lett 233(1–2):87–102. https://doi.org/10.1016/j.epsl.2005.02.003

2. Allègre CJ, Turcotte DL (1986) Implications of a two-component marble-cake mantle. Nature 323:123. https://doi.org/10.1038/323123a0

3. Anders E, Grevesse N (1989) Abundances of the elements: meteoritic and solar. Geochim Cosmochim Acta 53(1):197–214. https://doi.org/10.1016/0016-7037(89)90286-X

4. Basch V, Rampone E, Borghini G, Ferrando C, Zanetti A (2019) Origin of pyroxenites in the oceanic mantle and their implications on the reactive percolation of depleted melts. Contrib Mineral Petrol. https://doi.org/10.1007/s00410-019-1640-0

5. Batanova VG, Belousov IA, Savelieva GN, Sobolev AV (2011) Consequences of Channelized and Diffuse Melt Transport in Supra-subduction Zone Mantle: Evidence from the Voykar Ophiolite (Polar Urals). J Petrol 52(12):2483–2521. https://doi.org/10.1093/petrology/egr053

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