摘要
The muscovite in Hongzhen, Anhui Province, is identified as 2M1-phengite by x-ray diffraction and electron microprobe. Its structure, composition and paragenetic minerals imply medium pressure metamorphism.
The muscovite in Hongzhen, Anhui Province, is identified as 2M1-phengite by x-ray diffraction and electron microprobe. Its structure, composition and paragenetic minerals imply medium pressure metamorphism.
出处
《火山地质与矿产》
1995年第1期35-38,共4页
Volcanology & Mineral Resources
关键词
多硅白云母
安徽
变质岩系
白云母
phengite, medium pressure metamorphism, Hongzhen Area
