Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4741505 | Physics of the Earth and Planetary Interiors | 2015 | 10 Pages |
Abstract
We investigated the elastic anomalies of anorthite using molecular dynamics simulations in which the temperature and pressure induced P1¯/I1¯ phase transitions were reproduced. The resulting changes in structure were investigated as functions of pressure and temperature. It was found that the temperature-induced elastic anomaly is caused by two different thermal expansion behaviors of atomic motion, that is, increased distance between nearest neighbor atoms and increased Si–O–Al angle. Furthermore, the pressure-induced elastic anomaly was found to be caused by a decrease in the Si–O–Al angle in six-membered rings, which is similar to the cases of vitreous silica or acidic silicate liquids.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
Fumiya Noritake, Katsuyuki Kawamura, Kyoko N. Matsukage,