Upper‐Crustal Shear‐Wave Velocity Structure of the South‐Central Rio Grande Rift above the Socorro Magma Body Imaged with Ambient Noise by the Large‐N Sevilleta Seismic Array-Reference-Cited by-同舟云学术

Upper‐Crustal Shear‐Wave Velocity Structure of the South‐Central Rio Grande Rift above the Socorro Magma Body Imaged with Ambient Noise by the Large‐N Sevilleta Seismic Array

Published:2018-08-08 Issue:5 Volume:89 Page:1708-1719
ISSN:0895-0695
Container-title:Seismological Research Letters
language:en
Short-container-title:

Author:

Ranasinghe N. R.¹,Worthington L. L.¹,Jiang C.¹,Schmandt B.¹,Finlay T. S.¹,Bilek S. L.²,Aster R. C.³

Affiliation:

1. Department of Earth and Planetary Sciences, University of New Mexico, MSCO3‐2040, 1, Albuquerque, New Mexico 87131 U.S.A., nranasinghe@unm.edu

2. Department of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801 U.S. A.

3. Department of Geosciences, Warner College of Natural Resources, Colorado State University, 1482, Fort Collins, Colorado 80523 U.S.A.

Publisher

Seismological Society of America (SSA)

Subject

Geophysics

Link

https://pubs.geoscienceworld.org/ssa/srl/article-pdf/89/5/1708/4316926/srl-2018074.1.pdf

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