sporinite

基本解釋

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(rèn)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。
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.
烴源巖主要生烴顯微組分為基質(zhì)鏡質(zhì)體，少量孢子體、角質(zhì)體和碎屑?xì)べ|(zhì)體。
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(jì)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。
the fluorescence parameters of sporinite are important thermal maturity indicators, biomarker parameter are effective maturity indicator.
三塘湖盆地有機質(zhì)總體熱演化水平較低,且在橫向和縱向上存在明顯的差異。