Three‐Dimensional S Velocity Structure of the Mantle Transition Zone Beneath Central America and the Gulf of Mexico Inferred Using Waveform Inversion-Reference-Cited by-同舟云学术

Three‐Dimensional S Velocity Structure of the Mantle Transition Zone Beneath Central America and the Gulf of Mexico Inferred Using Waveform Inversion

Published:2019-09 Issue:9 Volume:124 Page:9664-9681
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Borgeaud Anselme F. E.¹²^ORCID,Kawai Kenji¹^ORCID,Geller Robert J.¹^ORCID

Affiliation:

1. Department of Earth and Planetary Science, School of Science University of Tokyo Tokyo Japan

2. Now at Institute of Earth Sciences Academia Sinica Taipei Taiwan

Funder

Japan Society for the Promotion of Science

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/10.1029/2018JB016924

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2. Compositional mantle layering revealed by slab stagnation at ~1000-km depth

3. Synthetic inversions for density using seismic and gravity data

4. Borgeaud A. F. E. Kawai K. &Geller R. J.(2019).Numerical parameters for 3‐D models presented in this paper available for download from the University of Tokyo Repository.http://doi.org/10.15083/00077029

5. Imaging paleoslabs in the D″ layer beneath Central America and the Caribbean using seismic waveform inversion

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