High Pressure‐Temperature Single‐Crystal Elasticity of Grossular: Implications for the Low‐Velocity Layer in the Bottom Transition Zone-Reference-Cited by-同舟云学术

High Pressure‐Temperature Single‐Crystal Elasticity of Grossular: Implications for the Low‐Velocity Layer in the Bottom Transition Zone

Published:2021-05-04 Issue:9 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Wei Wei¹,Mao Zhu¹²^ORCID,Sun Ningyu¹²^ORCID,Sun Daoyuan¹²^ORCID,Tkachev Sergey N.³^ORCID

Affiliation:

1. Laboratory of Seismology and Physics of Earth's Interior School of Earth and Planetary Sciences University of Science and Technology of China Hefei Anhui China

2. CAS Center for Excellence in Comparative Planetology University of Science and Technology of China Hefei Anhui China

3. Center for Advanced Radiation Sources University of Chicago Chicago IL USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL093540

Reference142 articles.

1. Elastic properties of garnet solid-solution series

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4. Elasticity of grossular and spessartite garnets by Brillouin spectroscopy

5. The Effect of Pressure Upon the Elastic Parameters of Isotropic Solids, According to Murnaghan's Theory of Finite Strain

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