The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
黄县盆地下第三系有机岩中
有丰富的壳质组和腐泥组,尤其发育
和藻类,这些富氢组分的荧光性质各不相同。
；；
；质The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
黄县盆地下第三系有机岩中有丰富的壳质组和腐泥组,尤其发育和藻类,这些富氢组分的荧光性质各不相同。
Resinite is a rich n1aceral in Teriary humic coal,boghead-cannel coal and oil shale fromHuangxian Coalfield.
黄县田第三纪腐殖、藻烛、油页岩显微组分富。
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