Shigeharu Naka, Tetsuya Kameyama, Suketoshi Ito, Michio Inagaki
Abstract
Abstract Morphological development of coesite crystal obtained at 550∼900°C under 23∼55 kb was strongly influenced by the state of aggregates of intermediate quartz. The sizes of quartz aggregates and coesite crystals decreased with increaseing pressure and with decreasing temperature.
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Abstract Morphological development of coesite crystal obtained at 550∼900°C under 23∼55 kb was strongly influenced by the state of aggregates of intermediate quartz. The sizes of quartz aggregates and coesite crystals decreased with increaseing pressure and with decreasing temperature.
Key concepts: Coesite, Quartz, Metastability, Chemistry, Crystallization, Crystal (programming language), Mineralogy, Crystallography