1．高圧鉱物（地球深部物質）
MgSiO3-FeAlO3系ペロブスカイトの固溶メカニズムと結晶化学
2011 年 53 巻 1 号 p. 8-12
詳細
2011 年 53 巻 1 号 p. 8-12
MgSiO3 dominant perovskite is believed to be the most abundant constituent mineral in the Earth’s lower mantle. Generally minerals form solid solutions and their nature should affect on physical properties of minerals. In this paper, we will introduce our recent studies about incorporation mechanism of FeAlO3 component into MgSiO3 perovskite and its crystal chemistry.
