在张小楼煤矿可以观察到丝质体(Fusinite)、粗粒体(Macrinite),徽粒 体(Micrinite),惰屑体(Inertodetrinite)和少量菌类体(Sclerotinite)
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rank fusinite 后生丝质体
fusinite splitter 碎屑丝质体
fusinite-telinite coal 丝质结构镜质煤
fusinite-collinite coal 丝质无结构镜质煤
fusinite-precollinite coal 丝质似结构镜质煤
fusinite-posttelinite coal 丝质亚结构镜质煤
fusinite needles 针状丝质体
semi fusinite 半丝质体
removing fusinite 丝炭脱除
Carbon and hydrogen contents of vitrinite to fusinite vary in one direction.
碳、氢含量由镜质组至丝质组呈单方向变化。
With increasing temperature, the yield of volatile matter of vitrinite and fusinite increased.
随热解温度升高，镜质组和丝质组的挥发分收率增加。
Concentrates of vitrinite, semi-vitrinite and fusinite are separated from Xinglong- zhuang coal by centrifugal method with heavy liquid.
通过重液离心分离法将兴隆庄煤分为镜质组、半镜质组、丝质组的富集物。
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