Evidence of Volatile‐Induced Melting in the Northeast Asian Upper Mantle-Reference-Cited by-同舟云学术

Evidence of Volatile‐Induced Melting in the Northeast Asian Upper Mantle

Published:2021-10 Issue:10 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Sun Yizhuo¹²³⁴^ORCID,Hier‐Majumder Saswata²⁵^ORCID,Tauzin Benoit⁶⁷^ORCID,Walter Michael⁸^ORCID,Ballmer Maxim⁹^ORCID,Xu Yigang¹³^ORCID,Kim Seongryong¹⁰^ORCID

Affiliation:

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

2. Department of Earth Sciences Royal Holloway University of London Egham UK

3. CAS Center for Excellence in Deep Earth Science Guangzhou China

4. University of Chinese Academy of Sciences Beijing China

5. Department of Energy AAAS Science and Technology Policy Fellow Advanced Scientific Computing Research Germantown MD USA

6. Université de Lyon Université Claude Bernard Lyon 1 Ecole Normale Supérieure de Lyon Université Jean Monnet CNRS LGL‐TPE Villeurbanne France

7. Research School of Earth Sciences Australian National University Canberra ACT Australia

8. Earth and Planets Laboratory Carnegie Institution for Science Washington DC WA USA

9. Department of Earth Sciences University College London London UK

10. Department of Earth and Environmental Sciences Korea University Seoul Republic of Korea

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Horizon 2020 Framework Programme

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/10.1029/2021JB022167

Reference95 articles.

1. Melting in the deep upper mantle oceanward of the Honshu slab

2. Experimental Melting of Carbonated Peridotite at 6-10 GPa

3. Mineral inclusions in sublithospheric diamonds from Collier 4 kimberlite pipe, Juina, Brazil: subducted protoliths, carbonated melts and primary kimberlite magmatism

4. Stable isotope evidence for crustal recycling as recorded by superdeep diamonds

5. The recycling of marine carbonates and sources of HIMU and FOZO ocean island basalts

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