The crystal structure at 220°C of orthorhombic high tridymite from the Steinbach meteorite

W. A. Dollase

doi:10.1107/s0365110x67003287

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The crystal structure at 220°C of orthorhombic high tridymite from the Steinbach meteorite

W. A. Dollase

Year: 1967 Journal: Acta Crystallographica Vol: 23 (4)Pages: 617-623 Publisher: Wiley

DOI: 10.1107/s0365110x67003287

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Keywords:

Tridymite Meteorite Orthorhombic crystal system Crystallography Materials science Achondrite Crystal structure Astrobiology Chemistry Physics Chondrite Metallurgy Cristobalite

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Astro and Planetary Science

Physical Sciences → Physics and Astronomy → Astronomy and Astrophysics

Planetary Science and Exploration

Physical Sciences → Physics and Astronomy → Astronomy and Astrophysics

High-pressure geophysics and materials

Physical Sciences → Earth and Planetary Sciences → Geophysics

The crystal structure at 220°C of orthorhombic high tridymite from the Steinbach meteorite

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