The equation of state of forsterite to 17.2 GPa and effects of pressure media-Reference-Cited by-同舟云学术

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The equation of state of forsterite to 17.2 GPa and effects of pressure media

Published:1996-02-01 Issue:1-2 Volume:81 Page:51-55
ISSN:0003-004X
Container-title:American Mineralogist
language:en
Short-container-title:American Mineralogist

Author:

Downs Robert T.,Zha Chang-Sheng,Duffy Thomas S.,Finger Larry W.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

Cited by 70 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. The effect of antigorite dehydration on velocity structure and water migration in subduction zones;Geoscience Frontiers;2024-09

2. Temperature and pressure effects on the structural and vibrational properties of forsterite from density functional theory studies;Physics and Chemistry of Minerals;2024-08-08

3. Sound velocities and single-crystal elasticity of hydrous Fo90 olivine to 12 GPa;Physics of the Earth and Planetary Interiors;2023-04

4. Adsorption behavior of molecular hydrogen in forsterite;Physics of the Earth and Planetary Interiors;2023-01

5. Hydration Effect on Equations of State for Minerals in the Peridotite System: Implication for Geotherms in the Mantle;Journal of Earth Science;2022-10

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