Geochemistry of metabasite in Mariana forearc serpentinite mudflows documents interactions between serpentinizing fluid and subducted seamount basalts-Reference-Cited by-同舟云学术

Geochemistry of metabasite in Mariana forearc serpentinite mudflows documents interactions between serpentinizing fluid and subducted seamount basalts

Published:2024-06 Issue: Volume:655 Page:122090
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Zhao Rui-Peng,Li Hong-Yan,Ryan Jeffrey G.,Wei Xun,Yang Sheng-Xiong,Xu Yi-Gang

Funder

National Natural Science Foundation of China

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

Publisher

Elsevier BV

Reference63 articles.

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2. Shallow depth, substantial change: fluid-metasomatism causes major compositional modifications of subducted volcanics (Mariana Forearc);Albers;Front. Earth Sci.,2022

3. Pb isotopic analysis of standards and samples using a 207Pb–204Pb double spike and thallium to correct for mass bias with a double-focusing MC-ICP-MS;Baker;Chem. Geol.,2004

4. Chemical and isotopic cycling in subduction zones;Bebout;Treat. Geochem.,2014

5. Boron isotope systematics of slab fuids as inferred from a serpentine Seamount, Mariana forearc;Benton;Earth Planet. Sci. Lett.,2001

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1. Serpentinite geochemistry documents the earliest dehydration and decarbonation of the subducting slab beneath the Mariana forearc;Earth and Planetary Science Letters;2024-07