Origin and multi-episodic melt/fluid interactions revealed by the subducted serpentinites in the North Qilian Belt, NW China: Implications for the compositional heterogeneity of the fossil oceanic mantle

Author:

Zhang Miao,Zhao JingORCID,Guo Jia,Chen Xi,Peng Xiuhong

Funder

Sichuan Provincial Science and Technology Support Program

Science and Technology Department of Sichuan Province

Chengdu University of Technology Key Laboratory of Applied Nuclear Techniques in Geosciences Sichuan

Northwest University

Publisher

Elsevier BV

Reference83 articles.

1. Variant across-forearc compositions of slab-fluids recorded by serpentinites: implications on the mobilization of FMEs from an active subduction zone (Mariana forearc);Albers;Lithos,2020

2. Mid-ocean ridge and supra-subduction geochemical signatures in spinel-peridotites from the Neotethyan ophiolites in SW Turkey: implications for upper mantle melting processes;Aldanmaz;Lithos,2009

3. BGQP (Bureau of Geology of Qinghai Province), 1968. The Geological Map (1:200000) of Yeniutai area (in Chinese).

4. Orogenic, ophiolitic, and abyssal peridotites;Bodinier;Treatise on Geochem.,2007

5. Nickel laterite ore deposits: weathered serpentinites;Butt;Elements,2013

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