摘要
对会理县的文石进行矿物学研究后,证实其成分接近理想的CaCO_3的文石晶体。并探讨了文石的形成机制。
Detailed examinations of chemical composition, X-ray diffraction, infrared spectrum, SEM and optical properties indicate that the crystals from Huili Sichuan province are aragonite which are nearly pure CaCC_3 in composition. The genesis of aragonite is also discussed in this paper.
出处
《矿物岩石》
CAS
CSCD
1992年第1期8-11,共4页
Mineralogy and Petrology
关键词
霞石
晶体
矿物学
红外吸收谱
Aragonite
infrared spectrum
metastability
