Vastly Different Heights of LLVPs Caused by Different Strengths of Historical Slab Push
Author:
Affiliation:
1. School of Earth and Space Exploration Arizona State University Tempe AZ USA
2. Now at Seismological Laboratory California Institute of Technology Pasadena CA USA
Funder
National Science Foundation
Division of Earth Sciences
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL099564
Reference78 articles.
1. Subducting-slab transition-zone interaction: Stagnation, penetration and mode switches
2. Compositional layering within the large low shear‐wave velocity provinces in the lower mantle
3. Mantle conveyor beneath the Tethyan collisional belt
4. Three-Dimensional Spherical Models of Convection in the Earth's Mantle
5. Modeling the Dynamics of Subducting Slabs
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