03aC07 隕石を構成するオリビン微粒子表面の形成環境(結晶評価・その場観察(1),第36回結晶成長国内会議)

概要

論文の詳細を見る
Formation process of matrix olivine surface microtopography was experimentally simulated Few μm sized 2-dimentional nucleation growth islands were observed on the surface. It was thought that the difference of the shape of step between sharp and rough depends on whether supersaturation excess the critical supersaturation or not Our experiment indicates that some matrix olivine remained the record that they cooled rapidly more than 500K/sec.
日本結晶成長学会の論文
2006-11-01