Phase relations of the Al2O3–SiO2 system at 13–21 GPa and 2300–2800 K and a new high-pressure Al2Si2O7 phase-Reference-Cited by-同舟云学术

Phase relations of the Al2O3–SiO2 system at 13–21 GPa and 2300–2800 K and a new high-pressure Al2Si2O7 phase

Published:2021-06-26 Issue:7 Volume:48 Page:
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Zhou Youmo^ORCID,Irifune Tetsuo,Kuribayashi Takahiro

Funder

Japan Society for the Promotion of Science

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

https://link.springer.com/content/pdf/10.1007/s00269-021-01149-3.pdf

Reference26 articles.

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2. Åsbrink S (1980) The crystal structure of and valency distribution in the low-temperature modification of V3O5. The decisive importance of a few very weak reflexions in a crystal-structure determination. Acta Cryst B36:1332–1339. https://doi.org/10.1107/S0567740880006036

3. Brown ID (1992) Chemical and steric constraints in inorganic solids. Acta Cryst B48:553–572. https://doi.org/10.1107/S0108768192002453

4. Farrugia LJ (1999) WinGX suite for small-molecule single-crystal crystallography. J Appl Crystallogr 32(4):837–838. https://doi.org/10.1107/S0021889899006020

5. Hazen RM (1976) Effects of temperature and pressure on the crystal structure of forsterite. American Mineralogist 61:1280–1293. https://pubs.geoscienceworld.org/msa/ammin/article-abstract/61/11-12/1280/40602/Effects-of-temperature-and-pressure-on-the-crystal?redirectedFrom=fulltext

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