alginite

基本解釋

The organic source rocks of Paleogene from Huangxian basin are rich in the content of exinite and sapropelinite,especially resinite and alginite.
黃縣盆地下第三系有機巖中含有豐富的殼質(zhì)組和腐泥組,尤其發(fā)育樹脂體和藻類體,這些富氫組分的熒光性質(zhì)各不相同。
Alginite and sporinite is suggested to be main macerals of hydrocarbon generation.Based on the study, a hydrocarbon generation model of source rocks in Subei basin is established.
確認藻類體和孢子體為其最主要的生烴組分，在此基礎(chǔ)上建立了蘇北盆地下第三系烴源巖的生烴模式。
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。