A Partial Molten Low‐Velocity Layer Atop the Mantle Transition Zone Beneath the Western Junggar: Implication for the Formation of Subduction‐Induced Sub‐Slab Mantle Plume-Reference-Cited by-同舟云学术

A Partial Molten Low‐Velocity Layer Atop the Mantle Transition Zone Beneath the Western Junggar: Implication for the Formation of Subduction‐Induced Sub‐Slab Mantle Plume

Published:2022-02 Issue:2 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Li Guohui¹^ORCID,Zhou Yuanze²^ORCID,Ding Lin³^ORCID,Gao Yuan¹^ORCID,Bai Ling³^ORCID,Zhang Heng³^ORCID,Hu Le¹,Pan Zhengyang¹,Ju Changhui¹^ORCID,Zhang Dingding³^ORCID

Affiliation:

1. Key Laboratory of Earthquake Prediction Institute of Earthquake Forecasting China Earthquake Administration Beijing China

2. Key Laboratory of Computational Geodynamics College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

3. State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment Chinese Academy of Sciences Beijing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC010150

Reference52 articles.

1. Whole-mantle convection and the transition-zone water filter

2. Upper mantlePvelocity structure beneath the Midwestern United States derived from triplicated waveforms

3. Upper-mantle velocity structures beneath the Tibetan Plateau and surrounding areas inferred from triplicated P waveforms

4. Deep upper-mantle melting beneath the Tasman and Coral Seas detected with multiple ScS reverberations

5. Intra-continental deformation and tectonic evolution of the West Junggar Orogenic Belt, Central Asia: Evidence from remote sensing and structural geological analyses

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1. Deep low velocity layer in the sublithospheric mantle beneath India;Geophysical Journal International;2024-08-06

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3. Hydrous Melting Driven Upwelling From the Mantle Transition Zone in the Mongolia Plateau Revealed by Receiver Function Analysis;Journal of Geophysical Research: Solid Earth;2022-11