Subduction‐Induced Upwelling of a Hydrous Transition Zone: Implications for the Cenozoic Magmatism in Northeast China
Author:
Affiliation:
1. State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics, Chinese Academy of Sciences Beijing China
2. Dipartimento di Geoscienze, Università di Padova Padova Italy
Funder
Horizon 2020 Framework Programme
National Basic Research Program of China
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/10.1029/2019JB018133
Reference84 articles.
1. Representing anisotropic subduction zones with isotropic velocity models: A characterization of the problem and some steps on a possible path forward
2. The effects of buoyancy on shear-induced melt bands in a compacting porous medium
3. Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China
4. Effects of mantle and subduction-interface rheologies on slab stagnation and trench rollback
5. Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation
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