角质煤素质
The results of fluorescence evalution of cutinite and suberinite show th... 煤中角质体和木栓质体的光性演化表明其对本区煤成油有一定的贡献。
Abundant cutinite and exitinite of oil shale cause the volume of long-chain saturated hydrocarbon increases. 油页岩中含有丰富的角质体和壳屑体，导致长链饱和烃增加。
A small quantity of sporinite and cutinite were identified in addition to the majority of the hydrocarbon-forming micro-components that mainly occurred as matrix vitrinites. 烃源岩主要生烃显微组分为基质镜质体，少量孢子体、角质体和碎屑壳质体。
Main macerals of hydrocarbon generation are sporinite, cutinite, alginite, bituminite, liptodetrinite and desmocollnite in source rocks from Jurassic coal measure in Northwest China. 西北地区侏罗纪煤系地层中主要的生烃显微组分是孢子体、角质体、藻类体、沥青质体、碎屑类脂体、基质镜质体等，而树脂体、木栓质体等早期低熟生油组分含量很低。
Whereas fusinite are dominant by aromatic structure.The study indicates that cutinite is one of the best oil source-rocks,with the higher hydrocarbon-generation potential; 镜质体结构组成介于角质体和丝质体之间
