Characteristics of deep crustal seismic anisotropy from a compilation of rock elasticity tensors and their expression in receiver functions-Reference-Cited by-同舟云学术

Characteristics of deep crustal seismic anisotropy from a compilation of rock elasticity tensors and their expression in receiver functions

Published:2017-09 Issue:9 Volume:36 Page:1835-1857
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Brownlee Sarah J.¹^ORCID,Schulte‐Pelkum Vera²^ORCID,Raju Anissha³,Mahan Kevin³^ORCID,Condit Cailey³^ORCID,Orlandini Omero Felipe³^ORCID

Affiliation:

1. Department of Geology Wayne State University Detroit Michigan USA

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

3. Department of Geological Sciences University of Colorado Boulder Boulder Colorado USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017TC004625

Reference89 articles.

1. The elastic properties of rock‐forming minerals: Pyroxenes and amphiboles;Aleksandrov K. S.;Bull. Acad. Sci. USSR Geophys. Ser.,1961

2. Elastic properties of rock‐forming minerals. II. Layered silicates;Aleksandrov K. S.;Bull. Acad. Sci. USSR Geophys. Ser.,1961

3. Elastic wave propagation in layered anisotropic media

4. Layered crustal anisotropy around the San Andreas Fault near Parkfield, California

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