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含有丰富的壳质组和腐泥组,尤其发育树脂体和藻体,这些富氢组的荧光质各不相同。
The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
黄县盆地下第三系有机岩中含有丰富的壳质组和腐泥组,尤其发育树脂体和藻体,这些富氢组的荧光质各不相同。
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