Oxidation Extent of the Upper Mantle by Subducted Slab and Possible Oxygen Budget in Deep Earth Inferred From Redox Kinetics of Olivine-Reference-Cited by-同舟云学术

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Oxidation Extent of the Upper Mantle by Subducted Slab and Possible Oxygen Budget in Deep Earth Inferred From Redox Kinetics of Olivine

Published:2022-02 Issue:2 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Zhao Chengcheng¹²^ORCID,Yoshino Takashi¹^ORCID,Zhang Baohua³^ORCID

Affiliation:

1. Institute for Planetary MaterialsOkayama UniversityMisasaJapan

2. Laboratoire Magmas et Volcans CNRSIRDOPGCUniversité Clermont AuvergneClermont‐FerrandFrance

3. Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang ProvinceInstitute of Geology and GeophysicsSchool of Earth SciencesZhejiang UniversityHangzhouChina

Funder

Ministry of Education, Culture, Sports, Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022977

Reference75 articles.

1. Experimental metamorphism of NaCl-bearing aqueous solutions by reactions with silicates

2. The redox budget of the Mariana subduction zone

3. Temporal evolution of mantle wedge oxygen fugacity during subduction initiation

4. Variations in Fe3+/∑Fe of Mariana Arc Basalts and Mantle Wedge fO2

5. The oxidation state of the Earth's sub-oceanic mantle from oxygen thermobarometry of abyssal spinel peridotites

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