Shear Velocity Model of Alaska Via Joint Inversion of Rayleigh Wave Ellipticity, Phase Velocities, and Receiver Functions Across the Alaska Transportable Array-Reference-Cited by-同舟云学术

Shear Velocity Model of Alaska Via Joint Inversion of Rayleigh Wave Ellipticity, Phase Velocities, and Receiver Functions Across the Alaska Transportable Array

Published:2020-02 Issue:2 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Berg Elizabeth M.¹^ORCID,Lin Fan‐Chi¹²^ORCID,Allam Amir¹^ORCID,Schulte‐Pelkum Vera³^ORCID,Ward Kevin M.⁴^ORCID,Shen Weisen⁵^ORCID

Affiliation:

1. Department of Geology and Geophysics University of Utah Salt Lake City UT USA

2. Institute of Earth Sciences Academia Sinica Taipei Taiwan

3. Cooperative Institute for Research in Environmental Sciences and Department of Geological Sciences University of Colorado Boulder Boulder CO USA

4. Department of Geology and Geological Engineering South Dakota School of Mines and Technology Rapid City SD USA

5. Department of Geosciences State University of New York at Stony Brook Stony Brook NY USA

Funder

National Science Foundation

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/10.1029/2019JB018582

Reference93 articles.

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2. Ten kilometer vertical Moho offset and shallow velocity contrast along the Denali fault zone from double-difference tomography, receiver functions, and fault zone head waves

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4. Cenozoic tectono-thermal history of the Tordrillo Mountains, Alaska: Paleocene-Eocene ridge subduction, decreasing relief, and late Neogene faulting

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