Aqueous Fluid Connectivity in Subducting Oceanic Crust at the Mantle Transition Zone Conditions-Reference-Cited by-同舟云学术

Aqueous Fluid Connectivity in Subducting Oceanic Crust at the Mantle Transition Zone Conditions

Author:

Liu Xingcheng¹²^ORCID,Matsukage Kyoko N.²³,Li Yuan^ORCID,Takahashi Eiichi¹²,Suzuki Toshihiro²,Xiong Xiaolin¹^ORCID

Affiliation:

1. State Key Laboratory of Isotope Geochemistry; Guangzhou Institute of Geochemistry, Chinese Academy of Sciences; Guangzhou China

2. Magma Factory, Department of Earth and Planetary Sciences; Tokyo Institute of Technology; Tokyo Japan

3. Center for Fundamental Education; Teikyo University of Science; Uenohara Japan

Funder

Chinese Academy of Sciences

Japan Society for the Promotion of Science

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

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

Link

Reference59 articles.

1. Density of MORB eclogite in the upper mantle;Aoki;Physics of the Earth and Planetary Interiors,2004

2. Water in the Earth's mantle;Bolfan-Casanova;Mineralogical Magazine,2005

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