The Continually Stable Subduction, Iron‐Spin Transition, and the Formation of LLSVPs From Subducted Oceanic Crust-Reference-Cited by-同舟云学术

The Continually Stable Subduction, Iron‐Spin Transition, and the Formation of LLSVPs From Subducted Oceanic Crust

Published:2020-01 Issue:1 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Huang Chuan¹²,Leng Wei¹³,Wu Zhongqing¹³

Affiliation:

1. Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Space Sciences University of Science and Technology of China Hefei China

2. Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences Peking University Beijing China

3. CAS Center for Excellence in Comparative Planetology Hefei China

Funder

National Natural Science Foundation of China-Yunnan Joint Fund

Chinese Academy of Sciences

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/10.1029/2019JB018262

Reference69 articles.

1. The growth of the continental crust: Constraints from zircon Hf-isotope data

2. Implications of melting for stabilisation of the lithosphere and heat loss in the Archaean

3. Deep storage of oceanic crust in a vigorously convecting mantle

4. Methods for thermochemical convection in Earth's mantle with force-balanced plates

5. Plume Generation Zones at the margins of Large Low Shear Velocity Provinces on the core–mantle boundary

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