Formation of Mg-Orthocarbonate through the Reaction MgCO3 + MgO = Mg2CO4 at Earth’s Lower Mantle P

Formation of Mg-Orthocarbonate through the Reaction MgCO3 + MgO = Mg2CO4 at Earth’s Lower Mantle P–T Conditions

Published:2021-04-22 Issue:5 Volume:21 Page:2986-2992
ISSN:1528-7483
Container-title:Crystal Growth & Design
language:en
Short-container-title:Crystal Growth & Design

Author:

Gavryushkin Pavel N.¹²^ORCID,Sagatova Dinara N.¹²,Sagatov Nursultan¹^ORCID,Litasov Konstantin D.³

Affiliation:

1. Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, prosp. acad. Koptyuga 3, 630090 Novosibirsk, Russian Federation

2. Novosibirsk State University, Pirogova 2, 630090 Novosibirsk, Russian Federation

3. Vereshchagin Institute for High Pressure Physics RAS, 108840 Troitsk, Moscow, Russian Federation

Funder

Russian Foundation for Basic Research

Publisher

American Chemical Society (ACS)

Subject

Condensed Matter Physics,General Materials Science,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/acs.cgd.1c00140

Reference53 articles.

1. Toward Analysis of Structural Changes Common for Alkaline Carbonates and Binary Compounds: Prediction of High-Pressure Structures of Li2CO3, Na2CO3, and K2CO3

2. High-Pressure Phase Diagrams of Na2CO3 and K2CO3

3. High-pressure structure of Li2CO3

4. High-pressure phases of CaCO3: Crystal structure prediction and experiment

5. Structures and stability of calcium and magnesium carbonates at mantle pressures

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