Through site observation and indoor measurements in XieJiaji No.2 Coal Mine in Huainan and Luling Coal Mine in Huaibei, it is discovered that the fragmentation degree are different in different coal seams in same mining district and even in sublevels of the are coal seam,tbe coal mass structures exist much difference. By analyzing the relationship between the constitution of coal matters and the epigenesis breakage of coal. This paper points out that the internal factor which causes the diversity of the coal mass structure are from the diversity in the contents of telocollinite and desmocollinite in the vitrinite. The contenet of desmocollinite is higher than that of telocollinite in intact coal seam (sublevel) but the former is less than the later in breaking sublevel, the diversity of constituent content more affects the epigenetic fragmtation degree of coal seam. The content of desmocollinite proves lower than that of telocollinite in the broken coal seam. The new understanding has directing, and reference for the study of coal perology, coal mine gas geology and coal methane.
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