Multiple crust-mantle interactions during tectonic development from oceanic subduction to continental collision: Constraints from mantle wedge serpentinites in a continental subduction zone-Reference-Cited by-同舟云学术

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Multiple crust-mantle interactions during tectonic development from oceanic subduction to continental collision: Constraints from mantle wedge serpentinites in a continental subduction zone

Published:2024-10 Issue: Volume:482-483 Page:107713
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Yin Zhuang-Zhuang,Chen Ren-Xu,Gong Bing,Zha Xiang-Ping

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

National Key Research and Development Program of China

Publisher

Elsevier BV

Reference80 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. Methane and propane micro-inclusions in olivine in titanoclinohumite-bearing dunites from the Sanbagawa high-P metamorphic belt, Japan: hydrocarbon activity in a subduction zone and Ti mobility;Arai;Earth Planet. Sci. Lett.,2012

3. Chemical and isotopic cycling in subduction zones;Bebout,2014

4. Oxygen isotope heterogeneity and disequilibria of olivine crystals in large volume Holocene basalts from Iceland: evidence for magmatic digestion and erosion of Pleistocene hyaloclastites;Bindeman;Geochim. Cosmochim. Acta,2008

5. High-pressure serpentinization and abiotic methane formation in metaperidotite from the Appalachian subduction, northern Vermont;Boutier;Lithos,2021

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