准噶尔盆地油气源、油气分布与油气系统
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中国石油天然气股份有限公司科学研究与技术开发项目(编号: 010109-3和06-01A-01-02)


Oil and Gas Source, Occurrence and Petroleum System in the Junggar Basin, Northwest China
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    摘要:

    准噶尔盆地是中国西部典型的多旋回叠合盆地,发育有石炭系、二叠系、三叠系、侏罗系、白垩系和古近系6套烃源岩,同时存在6大类原油和3大类天然气,广泛分布于盆地不同地区。西北缘原油总体相似,碳同位素组成轻(δ13C<-29‰)、胡萝卜烷、类异戊二烯烷烃、三环萜烷、伽马蜡烷丰富,甾烷以C28、C29为主,基本没有重排甾烷,为第二类原油,来源于二叠系湖相烃源岩。腹部绝大多数原油与西北缘原油相似,但胡萝卜烷、类异戊二烯烷烃、伽马蜡烷等有差异,来源于不同凹陷的二叠系湖相烃源岩;少量原油碳同位素组成重(δ13C -28‰~-26‰),Pr/Ph大于2.5,三环萜烷以C19、C20为主,藿烷丰富而伽马蜡烷极低,以C29规则甾烷及重排甾烷为主,为第四类原油,来源于侏罗系煤系烃源岩。东部存在5种类型原油,第一类原油碳同位素组成特别重(δ13C>-26‰),来源于石炭系烃源岩;第二类原油与腹部地区绝大多数原油十分相似,来源于二叠系湖相烃源岩;第三类原油碳同位素组成轻、重排甾烷、Ts、C29Ts及C30重排藿烷异常丰富,来源于中上三叠统湖相烃源岩;第四类原油源于侏罗系煤系烃源岩;混合类原油为二叠系、三叠系、侏罗系原油的混合,各自贡献平均分别为20%,15%和65%。南缘存在4类典型原油,为第二、第四、第五和第六类原油,其中第二、第四类分别源于二叠系和侏罗系;第五类原油碳同位素组成轻(δ13C<-29‰)、Pr/Ph<1.0、伽马蜡烷丰富且有两个异构体、Ts、C29Ts、C30重排藿烷、C27~C29异胆甾烷及C30甲基甾烷丰富,来源于白垩系湖相烃源岩;第六类原油主要为中低成熟原油,碳同位素组成δ13C -28‰~-26‰,C27、C28、C29甾烷呈“V”型分布,甲藻甾烷异常丰富,来源于古近系湖相烃源岩。准噶尔盆地天然气有油型气、混合气和煤型气,前两类主要来源于二叠系湖相烃源岩和石炭系海相烃源岩,煤型气主要来源于石炭系和侏罗系煤系烃源岩。不同类型油气分布与不同时代烃源灶具有良好对应关系:石炭系油气主要分布于陆东-五彩湾;二叠系油气主要分布于西北缘、腹部与东部;三叠系原油仅分布于东部;侏罗系原油主要分布于东部与南部;白垩系原油仅分布于南缘中部;古近系原油仅分布于南缘西部。按照盆地构造特征及不同时代烃源灶与油气关系,将准噶尔盆地划分为西部、中部、东部、南部及乌伦古5个油气系统及15个子油气系统。

    Abstract:

    The Junggar Basin is a typical polycyclic superimposed basin in the Northwest China, which develops six sets of source rocks (Carboniferous, Permian, Triassic, Jurassic, Cretaceous and Paleogene) and contains six gruops of crude oil and three types of natural gas. The crude oils in the Northwestern Margin are basically similar and belong to the Group II oil. They have light carbon isotopic composition (δ13C<-29‰) and abundant carotenoids, isoprenoids, tricyclic terpanes and gammacerane. Steranes are dominated by C28 and C29 and there is nearly no diasteranes. These crude oils were derived from the Permian lacustrine source rocks. Most of the crude oils in the Central region of the basin are similar to those in the Northwestern Margin, but have difference in content of carotenoids, isoprenoids and gammacerane, which can be divided into four subgroups. These oils were derived from the Permian source rocks in different depressions. A small amount of crude oil has a heavy carbon isotopic composition (δ13C: -28‰ – -26‰) and Pr/Ph>2.5. The tricyclic terpane is mainly composed of C19 and C20. The hopanes are abundant but the gammacerane is extremely low. The steranes are mainly composed of C29 regular steranes and diasteranes. The oil was sourced from the Jurassic coal measures. There are five groups of crude oils in the Eastern Junggar. Group I crude oils have a very heavy carbon isotopic composition (δ13C>-26‰) and were derived from the Carboniferous source rocks. Group II crude oils are very similar to most of those in the Central region and were derived from the Permian lacustrine source rocks. Group III crude oils have a light carbon isotopic composition and are abundant in diasterane, Ts, C29Ts and C30 diahopane. They were derived from the Triassic lacustrine source rocks. Group IV crude oils come from the Jurassic coal measures. The mixed crude oil is a mixture of the Jurassic, Triassic and Permian oils, meanly accounting for 65%, 15% and 20%, respectively. There are four groups of typical crude oils in the Southern Margin, which belong to the Group II, IV, V and VI of crude oil, respectively. Group II and Group IV crude oils were derived from the Permian lacustrine source rocks and the Jurassic coal measures, respectively. Group V crude oils have a light carbon isotopic composition (δ13C<-29‰) and Pr/Ph<1.0. The gammacerane is abundant and has two isomers. The Ts, C29Ts, C30 diahopane, C27–C29 cholestanes and C30 methlysteranes are also abundant. They are derived from the Cretaceous lacustrine source rocks. Group VI crude oils, mainly low to medium mature oils, have a heavy carbon isotopic composition (δ13C: -28‰ – -26‰). The C27, C28 and C29 steranes are distributed in a V-shape. The dinosteranes are extremely abundant. They are derived from the Eocene lacustrine source rocks. Natural gas in the Junggar basin can be divided into three types, i.e. oil-derived, mixed and coal-derived. The first two types mainly come from the Permian lacustrine source rocks and the Carboniferous marine source rocks. The coal-derived gas comes mainly from the Carboniferous and Jurassic coal measures. The distribution of different types of oil and gas in the Junggar corresponds to the source kitchen developed in different geological ages. The Carboniferous oil and gas are mainly distributed in the Ludong-Wucaiwan area; the Permian oil and gas are widely distributed, mainly in the Northwestern Margin, the Central region and the Eastern area; the Triassic crude oil is limited to the Eastern area; the Jurassic crude oil is mainly distributed in the Eastern and Southern areas; the Cretaceous crude oil is mainly distributed in the middle of the Southern Margin; the Paleogene crude oil is mainly distributed in the western part of the Southern Margin. The Junggar basin can be divided into 5 petroleum systems, i.e. the Western, Central, Eastern, Southern and Ulungur petroleum systems, and 15 petroleum subsystems based on the structural features of the basin and the relations between source kitchens of different geolpgical ages and different types of oil and gas.

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陈建平,王绪龙,邓春萍,梁狄刚,张越迁,赵喆,倪云燕,支东明,杨海波,王屿涛.2016.准噶尔盆地油气源、油气分布与油气系统[J].地质学报,90(3):421-450.
Chen Jianping, Wang Xulong, Deng Chunping, Liang Digang, Zhang Yueqian, Zhao Zhe, Ni Yunyan, Zhi Dongming, Yang Haibo, Wang Yutao.2016. Oil and Gas Source, Occurrence and Petroleum System in the Junggar Basin, Northwest China[J]. Acta Geologica Sinica,90(3):421-450.

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  • 收稿日期:2015-03-24
  • 最后修改日期:2015-07-01
  • 录用日期:2015-07-02
  • 在线发布日期: 2016-03-14
  • 出版日期: