| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1753660 | International Journal of Coal Geology | 2012 | 21 Pages |
Abstract
⺠High proportions of diaspore, ammonian illite, and gorceixite were found in coal. ⺠Diaspore was derived from gibbsite dehydration due to the heat of igneous intrusions. ⺠Ammonian illite formed by interaction of kaolinite and nitrogen released from coal. ⺠The calcite and dolomite were derived from the igneous fluids.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
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Authors
Shifeng Dai, Jianhua Zou, Yaofa Jiang, Colin R. Ward, Xibo Wang, Tian Li, Weifeng Xue, Shande Liu, Heming Tian, Xinhao Sun, Dao Zhou,