Origin and accumulation mechanisms of petroleum in the Carboniferous volcanic rocks of the Kebai Fault zone, Western Junggar Basin, China

被引:29
作者
Chen, Zhonghong [1 ]
Zha, Ming [1 ]
Liu, Keyu [1 ]
Zhang, Yueqian [2 ]
Yang, Disheng [2 ]
Tang, Yong [2 ]
Wu, Kongyou [1 ]
Chen, Yong [1 ]
机构
[1] China Univ Petr, Sch Geosci, Changjiang West Rd 66, Qingdao 266580, Shandong, Peoples R China
[2] CNPC, Xinjiang Oilfield, Petr Explorat & Dev Res Inst, Karamay 834000, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Volcanic rock; Carboniferous; Reservoir; Diagenesis; Petroleum filling history; Petroleum accumulation; Petroleum origin; Junggar Basin; ASIAN OROGENIC BELT; NORTHERN QAIDAM BASIN; BOHAI BAY BASIN; TECTONIC EVOLUTION; NW CHINA; FLUID INCLUSIONS; SR-ND; GEOCHEMICAL CHARACTERISTICS; CONTINENTAL GROWTH; INTRUSIVE ROCKS;
D O I
10.1016/j.jseaes.2016.06.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Kebai Fault zone of the West Junggar Basin in northwestern China is a unique region to gain insights on the formation of large-scale petroleum reservoirs in volcanic rocks of the western Central Asian Orogenic Belt. Carboniferous volcanic rocks are widespread in the Kebai Fault zone and consist of basalt, basaltic andesite, andesite, tuff, volcanic breccia, sandy conglomerate and metamorphic rocks. The volcanic oil reservoirs are characterized by multiple sources and multi-stage charge and filling history, characteristic of a complex petroleum. system. Geochemical analysis of the reservoir oil, hydrocarbon inclusions and source rocks associated with these volcanic rocks was conducted to better constrain the oil source, the petroleum filling history, and the dominant mechanisms controlling the petroleum accumulation. Reservoir oil geochemistry indicates that the oil contained in the Carboniferous volcanic rocks of the Kebai Fault zone is a mixture. The oil is primarily derived from the source rock of the Permian Fengcheng Formation (P(1)f), and secondarily from the Permian Lower Wuerhe Formation (P(2)w). Compared with the P(2)w source rock, P(1)f exhibits lower values of C-19 IT/C-23 TT, C19+20TT/Sigma TT, Ts/(Ts + Tm) and alpha alpha alpha-20R sterane C-27/C-28 ratios but higher values of TT C-23/C-21, HHI, gammacerane/alpha beta C-30 hopane, hopane (20S) C-34/C-33, C-29 beta beta/(beta beta + alpha alpha), and C-29 20S/(20S + 20R) ratios. Three major stages of oil charge occurred in the Carboniferous, in the Middle Triassic, Late Triassic to Early Jurassic, and in the Middle Jurassic to Late Jurassic periods, respectively. Most of the oil charged during the first stage was lost, while moderately and highly mature oils were generated and accumulated during the second and third stages. Oil migration and accumulation in the large-scale stratigraphic reservoir was primarily controlled by the top Carboniferous unconformity with better porosity and high oil enrichment developed near the unconformity. Secondary dissolution pores and fractures are the two major reservoir storage-space types in the reservoirs. Structural highs and reservoirs near the unconformity are two favorable oil accumulation places. The recognition of the large-scale Carboniferous volcanic reservoirs in the Kebai Fault zone and understanding of the associated petroleum accumulation mechanisms provide new insights for exploring various types of volcanic reservoir plays in old volcanic provinces, and will undoubtedly encourage future oil and gas exploration of deeper strata in the region and basins elsewhere with similar settings. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:170 / 196
页数:27
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