Hydrous Melting Driven Upwelling From the Mantle Transition Zone in the Mongolia Plateau Revealed by Receiver Function Analysis-Reference-Cited by-同舟云学术

Hydrous Melting Driven Upwelling From the Mantle Transition Zone in the Mongolia Plateau Revealed by Receiver Function Analysis

Author:

He Jing¹²^ORCID,Xu Mijian³⁴^ORCID,Wu Qingju⁵^ORCID,Zhang Fengxue⁵^ORCID

Affiliation:

1. National Institute of Natural Hazards Ministry of Emergency Management of China Beijing China

2. Key Laboratory of Compound and Chained Natural Hazards Dynamics Ministry of Emergency Management of China Beijing China

3. Division of Mathematical Sciences School of Physical and Mathematical Sciences Nanyang Technological University Singapore Singapore

4. Earth Observatory of Singapore Nanyang Technological University Singapore Singapore

5. Institute of Geophysics China Earthquake Administration Beijing China

Funder

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

Reference62 articles.

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