Temporal and spatial mineralogical changes in clasts from Mariana serpentinite mud volcanoes: Cooling of the hot forearc-mantle at subduction initiation-Reference-Cited by-同舟云学术

Temporal and spatial mineralogical changes in clasts from Mariana serpentinite mud volcanoes: Cooling of the hot forearc-mantle at subduction initiation

Published:2021-03 Issue: Volume:384-385 Page:105941
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Ichiyama Yuji,Tsujimori Tatsuki,Fryer Patricia,Michibayashi Katsuyoshi,Tamura Akihiro,Morishita Tomoaki

Funder

Japan Agency for Marine-Earth Science and Technology

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference72 articles.

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3. Insights into petrological characteristics of the lithosphere of mantle wedge beneath arcs through peridotite xenoliths: a review;Arai;J. Petrol.,2008

4. Petrogenesis of serpentinites from the Franciscan complex, western California, USA;Barnes;Lithos,2013

5. Derivation of internally-consistent thermodynamic data by the technique of mathematical programming: a review with application to the system MgO-SiO2-H2O;Berman;J. Petrol.,1986

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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

2. Geochemistry of metabasite in Mariana forearc serpentinite mudflows documents interactions between serpentinizing fluid and subducted seamount basalts;Chemical Geology;2024-06

3. Two-stage exhumation of high-pressure rocks by corner flow and mud volcanism within an active subduction zone – A case study from serpentinite mud volcanoes along the Mariana convergent margin;Earth and Planetary Science Letters;2024-06

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5. Molybdenum Isotopic Signatures of Forearc Serpentinites: Origin and Contribution to the Subduction Zone Mo Cycle;Journal of Geophysical Research: Solid Earth;2024-02