Orthorhombic perovskite phases observed in olivine, pyroxene and garnet at high pressures and temperatures-Reference-Cited by-同舟云学术

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Orthorhombic perovskite phases observed in olivine, pyroxene and garnet at high pressures and temperatures

Published:1976-06 Issue:4 Volume:11 Page:289-298
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Liu Lin-Gun

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference19 articles.

1. Stishovite, SiO2, a very high pressure new mineral from Meteor Crater, Arizona

2. Synthesis of γ-Mg2SiO4

3. On the Materials and Density of the Earth's Crust.

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1. Disproportionation of Iron in Almandine‐Pyrope‐Grossular Garnet From 25 to 65 GPa;Geochemistry, Geophysics, Geosystems;2023-10

2. Diamonds reveal subducted slab harzburgite in the lower mantle;Geology;2023-01-20

3. Basics of Geochemistry and Mineralogy of Chromium;Geochemistry of Chromium in the Earth’s Mantle;2019-09-01

4. Chromium-bearing phases in the Earth's mantle: Evidence from experiments in the Mg2SiO4–MgCr2O4 system at 10–24 GPa and 1600°C;American Mineralogist;2018-01-01

5. Nomenclature of the perovskite supergroup: A hierarchical system of classification based on crystal structure and composition;Mineralogical Magazine;2017-06

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