High‐Pressure Single‐Crystal Elasticity and Thermal Equation of State of Omphacite and Their Implications for the Seismic Properties of Eclogite in the Earth's Interior-Reference-Cited by-同舟云学术

High‐Pressure Single‐Crystal Elasticity and Thermal Equation of State of Omphacite and Their Implications for the Seismic Properties of Eclogite in the Earth's Interior

Published:2019-03 Issue:3 Volume:124 Page:2368-2377
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Hao Ming¹^ORCID,Zhang Jin S.¹²^ORCID,Pierotti Caroline E.¹³,Ren Zhiyuan¹,Zhang D.⁴⁵^ORCID

Affiliation:

1. Department of Earth and Planetary Sciences University of New Mexico Albuquerque NM USA

2. Institute of Meteoritics University of New Mexico Albuquerque NM USA

3. Albuquerque High School Albuquerque NM USA

4. Hawaii Institute of Geophysics and Planetology University of Hawai‘i at Mānoa Honolulu HI USA

5. GeoSoiEnviroCARS University of Chicago, Argonne National Laboratory Argonne IL USA

Funder

University of New Mexico

Argonne National Laboratory

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/10.1029/2018JB016964

Reference73 articles.

1. Eclogite as a seismic marker in subduction channels: Seismic velocities, anisotropy, and petrofabric of Cabo Ortegal eclogite tectonites (Spain);Ábalos B.;Bulletin,2011

2. Gabbro-eclogite reaction rate and its geophysical significance

3. New Theory of the Earth

4. Anharmonicity and the equation of state for gold

5. 40 years of mineral elasticity: a critical review and a new parameterisation of equations of state for mantle olivines and diamond inclusions

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