角質(zhì)煤素質(zhì)

The results of fluorescence evalution of cutinite and suberinite show th... 煤中角質(zhì)體和木栓質(zhì)體的光性演化表明其對本區(qū)煤成油有一定的貢獻(xiàn)。

Abundant cutinite and exitinite of oil shale cause the volume of long-chain saturated hydrocarbon increases. 油頁巖中含有豐富的角質(zhì)體和殼屑體，導(dǎo)致長鏈飽和烴增加。

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. 烴源巖主要生烴顯微組分為基質(zhì)鏡質(zhì)體，少量孢子體、角質(zhì)體和碎屑?xì)べ|(zhì)體。

Main macerals of hydrocarbon generation are sporinite, cutinite, alginite, bituminite, liptodetrinite and desmocollnite in source rocks from Jurassic coal measure in Northwest China. 西北地區(qū)侏羅紀(jì)煤系地層中主要的生烴顯微組分是孢子體、角質(zhì)體、藻類體、瀝青質(zhì)體、碎屑類脂體、基質(zhì)鏡質(zhì)體等，而樹脂體、木栓質(zhì)體等早期低熟生油組分含量很低。

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; 鏡質(zhì)體結(jié)構(gòu)組成介于角質(zhì)體和絲質(zhì)體之間