Complexions and stoichiometry of the 60.8°//[100](011) symmetrical tilt grain boundary in Mg2SiO4 forsterite: A combined empirical potential and first-principles study
Author:
Affiliation:
1. Université de Lille, CNRS, INRAE, Centrale Lille, UMR 8207 - UMET - Unité Matériaux et Transformations, F-59000 Lille, France
2. Institut Universitaire de France, 1 rue Descartes, F-75005 Paris, France
Abstract
Publisher
Mineralogical Society of America
Subject
Geochemistry and Petrology,Geophysics
Link
https://pubs.geoscienceworld.org/msa/ammin/article-pdf/107/11/2034/5725980/am-2022-8420.pdf
Reference52 articles.
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2. Atoms in Molecules: A Quantum Theory;Bader,1990
3. The effects of both deviation from stoichiometry and boron on grain boundaries in Ni3Al;Baker;Philosophical Magazine B,1990
4. Why should we be interested in the atomic structure of interfaces?;Balluffi,1996
5. Microstructural evidence for grain boundary migration and dynamic recrystallization in experimentally deformed forsterite aggregates;Bollinger;Minerals,2018
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1. Structures and energies of twist grain boundaries in Mg2SiO4 forsterite;Computational Materials Science;2024-01
2. Metamorphic reaction kinetics at anhydrous to water-saturated conditions in the binary MgO-SiO2 system;Contributions to Mineralogy and Petrology;2023-11-16
3. The Role of Grain Boundaries in Low‐Temperature Plasticity of Olivine Revealed by Nanoindentation;Journal of Geophysical Research: Solid Earth;2023-08
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