Petrogenesis of the pyroxenitic Moho transition zone in the Zedong ophiolite, Southeastern Tibet-Reference-Cited by-同舟云学术

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Petrogenesis of the pyroxenitic Moho transition zone in the Zedong ophiolite, Southeastern Tibet

Published:2024-10 Issue: Volume:482-483 Page:107703
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

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

Funder

National Science Foundation

National Natural Science Foundation of China National Outstanding Youth Science Fund Project

Publisher

Elsevier BV

Reference91 articles.

1. The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both?;Abily;Geology,2013

2. Petrologic profile of peridotite layers under a possible Moho in the northern Oman ophiolite: An example from Wadi Fizh;Akizawa;J. Miner. Petrol. Sci.,2009

3. Behavior of MORB magmas at uppermost mantle beneath a fast-spreading axis: an example from Wadi Fizh of the northern Oman ophiolite;Akizawa;Contrib. Mineral. Petrol.,2012

4. Mantle wehrlite from Hess deep as a crystal cumulate from an ultra-depleted primary melt in East Pacific rise;Arai;Geophys. Res. Lett.,2007

5. Whole-rock and mineral chemistry of cumulates from the Kızıldağ (Hatay) ophiolite (Turkey): clues for multiple magma generation during crustal accretion in the southern Neotethyan Ocean;Bağci;Mineral. Mag.,2005

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