The mineralogical characteristics and genesis of the dickite in Taiyuan Formation in Southeastern Shanxi
The minerals in the partings of NO.15 Coal in Southeastern Shanxi were studied with X ray diffraction qualitative and quantitative analysis. The results indicated that the main clay minerals in the partings included dickite, ammonium illite and kaolinite, with a few illite and chlorite. The dickite was mainly distributed in the middle partings, pertain to 2M1 type, with the concentration of 34-78％, and the main diffraction peaks between 34°39°/26 were two pairs of peaks. The FWHM of basal diffraction peaks was relatively large, indicating lower crystallinity. The dickite of the research area was transformed form kaolinite during diagenesis and the generation temperature was 140°C more or less.
Southeastern Shanxi partings dickite Main text
Zheng Qiming Liu Qinfu Shen Qi Wu Zeguang Zhang Yinmin
School of Geological Science and Survey Engineering, China University of Mining and Technology, Beijing 100083, China
国际会议
The First International Symposium on Mine Safety Science and Engineering (首届矿山安全科学与工程学术会议)
北京
英文
946-949
2011-10-27（万方平台首次上网日期，不代表论文的发表时间）