Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography

Author:

Portner Daniel Evan12,Rodríguez Emily E.1,Beck Susan1,Zandt George1,Scire Alissa3,Rocha Marcelo P.4,Bianchi Marcelo B.5,Ruiz Mario6,França George Sand4,Condori Cristobal4,Alvarado Patricia7

Affiliation:

1. Department of Geosciences University of Arizona Tucson AZ USA

2. Now at Department of Terrestrial Magnetism Carnegie Institution for Science Washington DC USA

3. IRIS PASSCAL Instrument Center New Mexico Institute of Mining and Technology Socorro NM USA

4. Instituto de Geociências Universidade de Brasília Brasília Brazil

5. Centro de Sismologia, Departamento de Geofísica, Instituto de Geofísica, Astronomia, e Ciências Atmosféricas Universidade de São Paulo São Paulo Brazil

6. Instituto Geofísico Escuela Politécnica Nacional Quito Ecuador

7. Consejo Nacional de Investigaciones Científicas y Técnicas, Departamento de Geofísica y Astronomía, Facultad de Ciencias Exactas, Físicas y Naturales Universidad Nacional de San Juan San Juan Argentina

Funder

Division of Earth Sciences

University of Arizona

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference175 articles.

1. Crustal structure of the Amazonian Craton and adjacent provinces in Brazil

2. Albuquerque Seismological Laboratory (ASL)/USGS(1988).Global Seismograph Network (GSN ‐ IRIS/USGS).https://doi.org/10.7914/SN/IU

3. Seismic, Volcanic, and Geodetic Networks in Ecuador: Building Capacity for Monitoring and Research

4. Albuquerque Seismological Laboratory (ASL)/USGS(1993) Global Telemetered Seismograph Network (USAF/USGS).https://doi.org/10.7914/SN/GT

5. A lithospheric velocity model for the flat slab region of Argentina from joint inversion of Rayleigh wave phase velocity dispersion and teleseismic receiver functions

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