The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
县盆地下第三系有机岩中含有丰富的壳质组和腐泥组,尤其发育树脂
和藻类
,这些富
组分的荧光性质各不相同。
The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
县盆地下第三系有机岩中含有丰富的壳质组和腐泥组,尤其发育树脂
和藻类
,这些富
组分的荧光性质各不相同。
The main hydrocarbon-generating macerals in the source rocks of the coal measures are exinite, alginite and desmocollinite.Organic matter is dominantly of type III kerogen.
煤系烃源岩中主要的成烃显微组分是壳质、藻类
、基质镜质
,有机质类型以Ⅲ型为主;
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