摘要
根据分子有机地球化学理论,借助色谱和色质等先进测试手段,对赤峰盆地元宝山凹陷6个油样进行了分析研究。结果表明,元宝山凹陷的原油属重质稠油成熟度低生源物质以菌类和藻类微生物为主,后者大于前者;其生源物质形成于半咸水咸水湖相还原环境。利用有机显微组分荧光光谱研究了本区烃源岩的成烃机制,认为原油是生物类脂物早期生烃的产物。还对原油的稠化机理进行了分析认为可能是由其生源物质决定的,而后期又受轻微生物降解的影响,这与前人的研究成果迥然不同。同时,将本区原油与其他熟知的典型稠油进行对比,突出了本区原油的特殊性。
Six oil samples(2oil and 4oil sand samples)from Yuanbaoshan Depression,Chife ng Basin are analyzed based on the theory of molec ular organic geochemistry and by gas chromatography and gas chromatography-mass spectrometry(GC and GC-MS ).The results show that the oil is heavy-viscous crude oil with low maturity.Their organic precurs ors derived mainly from bacteria and alga of low microorganism,and forme d in brackish-saline lake reduction environment.The hydrocarbon-generating mechanism of the source rocks in t he study area is studied by maceral fluoresce ne spectrum,and it can be concluded t hat the oil is an early hydrocarbon-generating product of organism lipidal matter.Viscosify of the oil is controlled by organic pr ecursors and the viscous oil is probably of primary origin(only possibly affected slightly by b iodegradation),which differ greatly from the conclusion drawn pr eviously.The oil in the study area has its own characteristics compared with the typical known heavy-viscous crude o ils.
出处
《地球化学》
CAS
CSCD
北大核心
2001年第4期375-382,共8页
Geochimica
基金
华北油田资助项目
关键词
重质稠油生物类脂物
生源物质
成烃机制
赤峰盆地
元宝山凹陷
成熟度
heavy-viscous crude oil
organic li pidal matter
organic precursor
hydrocarbon-generating mechanism
Chifeng Basin