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对本区煤成油有一定的贡献。
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对本区煤成油有一定的贡献。
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
,
脂体、木栓质体
早期低熟生油组分含量很低。
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.
源岩主要生
显微组分为基质镜质体,少量孢子体、角质体和碎屑壳质体。
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