ミクロひずみを持つ微小鉱物の構造解析―天然の鉱物へのアプローチー
2001 年 43 巻 1 号 p. 81-83
詳細
2001 年 43 巻 1 号 p. 81-83
Natural crystal samples such as Fe-rich pumpellyite occurring in low-grade metamorphic rocks are composed of very fine grains and the crystalline quality of each grain is quite low. The Weissenberg method combined with imaging plate and synchrotron radiation as an X-ray source was employed to determine the crystal structure with low crystalline quality.
