松辽盆地齐家地区“四史”模拟及其地质意义研究
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摘要
为确定齐家地区高台子油层的油气成藏规律,应用IES petromod成藏模拟软件开展了地层埋藏史、压力演化史、成熟度演化史及油气运聚史"四史"模拟工作。地层埋藏史模拟结果表明:齐家地区经历了"3降2升"的地质埋藏过程,三个沉降期分别是:泉头组沉积末期-嫩江组沉积末期、四方台组-明水组沉积末期及依安组沉积末期-现今,两次构造抬升时期是嫩江组沉积末期、明水组沉积末期-依安组沉积末期。地层压力演化具有幕式的变化特征,青山口组二+三段地层随着埋深的增加,地层压力在嫩江组沉积末期达到峰值,后因嫩末构造运动的影响,地层压力开始减小,其后,又随着地层埋深的增加,地层压力逐渐增大,开始另一幕的形成,在明水组沉积末期,地层压力达到最大。成熟度演化史表明:嫩三段-嫩四段沉积时期,青一段烃源岩开始进入生烃门限,到明水组沉积末期,齐家-古龙凹陷一带烃源岩的镜质体反射率高达1. 0%～1. 3%,有机质成熟的范围也进一步扩大。油气运聚史表明,齐家地区高台子油层主要有嫩江组沉积末期、明水组沉积末期两次油气运聚成藏过程,其中明水组沉积末期,油气运聚范围最广,油气由生烃中心齐家-古龙凹陷向其两侧进行大规模的侧向运移聚集,形成了环凹陷周边的一系列油气藏。
To reveal the law of oil and gas accumulation of the Gaotaizi oil layer in the Qijia area,Songliao basin,this work has conducted simulations of histories of strata burial process,stratum pressure evolution,maturity change and hydrocarbon migration using IES Petromod software. Results show that the Qijia area has undergone"three subsidence and two uplifts"in the burial process,which were in K_1q-K_2n_5,K_2s-K_2m and Ey-Q for subsidence and end of K_2n_5 and end of K_2m-Ey for uplift,respectively. The evolution of formation pressure was characterized by episodic changes. With the increase of buried depth,formation pressure of K_2qn_2 + 3 reached the first overpressure peak at the end of the K_2n_5. Affected by the tectonic movement of the late K_2n_5,the formation pressure began to decrease gradually. Subsequently,with the increase of the depth of strata,the formation pressure gradually increased again and another episode began. At the end of sedimentation of K_2m,the formation pressure reached the maximum. During the period of K_2n_3-K_2n_4,the source rocks of K_1qn_1 began to enter the threshold of hydrocarbon generation. By the end of K_2m,the reflectance of the K_1qn_1 source rocks of the Qijia-Gulong sag was as high as 1. 0% ～ 1. 3%,and the range of organic maturation was further enlarged. The simulated history of oil and gas hydrocarbon migration and accumulation shows that the late stages of K_2n_5 and K_2m were two periods of accumulation of oil and gas in the Gaotaizi oil layer. Of them,at the end of K_2m,petroleum migration and accumulation were the most widespread,when large-scale oil and gas from the Qijia-Gulong depression hydrocarbon generation center moved to either side,forming a series of reservoirs surrounding the depression.
To reveal the law of oil and gas accumulation of the Gaotaizi oil layer in the Qijia area,Songliao basin,this work has conducted simulations of histories of strata burial process,stratum pressure evolution,maturity change and hydrocarbon migration using IES Petromod software. Results show that the Qijia area has undergone"three subsidence and two uplifts"in the burial process,which were in K_1q-K_2n_5,K_2s-K_2m and Ey-Q for subsidence and end of K_2n_5 and end of K_2m-Ey for uplift,respectively. The evolution of formation pressure was characterized by episodic changes. With the increase of buried depth,formation pressure of K_2qn_2 + 3 reached the first overpressure peak at the end of the K_2n_5. Affected by the tectonic movement of the late K_2n_5,the formation pressure began to decrease gradually. Subsequently,with the increase of the depth of strata,the formation pressure gradually increased again and another episode began. At the end of sedimentation of K_2m,the formation pressure reached the maximum. During the period of K_2n_3-K_2n_4,the source rocks of K_1qn_1 began to enter the threshold of hydrocarbon generation. By the end of K_2m,the reflectance of the K_1qn_1 source rocks of the Qijia-Gulong sag was as high as 1. 0% ～ 1. 3%,and the range of organic maturation was further enlarged. The simulated history of oil and gas hydrocarbon migration and accumulation shows that the late stages of K_2n_5 and K_2m were two periods of accumulation of oil and gas in the Gaotaizi oil layer. Of them,at the end of K_2m,petroleum migration and accumulation were the most widespread,when large-scale oil and gas from the Qijia-Gulong depression hydrocarbon generation center moved to either side,forming a series of reservoirs surrounding the depression.
引文
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Li Lei,Zuo Yinhui,Tang Shuheng,Zhang Songhang.2016.Cenozoic thermal history of the Dongpu sag,Bohai Bay basin[J].Geology and Exploration,52(3):594-600(in Chinese with English abstract).
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Sun Yu,Dong Yiming,Wang Jiping,Ma Shizhong,Yu Liming,Yan Baiquan.2016.Distribution patterns of single sand body in Fuyu oil layer in the northern Honggang area,Songliao basin[J].Lithologic Reservoirs,28(4):9-15(in Chinese with English abstract).
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Gao Ruiqi,Cai Xiyuan.1997.The reservoir distribution rules and formation condition of Songliao basin[M].Beijing:Petroleum Industry Press:1-319(in Chinese).
He Lijuan.2000.Advance in tectono-thermal modeling of sedimentary basins[J].Advances in Earth Science,15(6):661-665(in Chinese).
Hao Fang,Zou Huayao,Jiang Jianqun.2000.Dynamics of petroleum accumulation and its advances[J].Earth Science Frontiers,7(3):11-21(in Chinese with English abstract).
Hou Qijun,Feng Zhiqiang,Feng Zihui.2009.Terrestrial petroleum geology of Songliao basin[M].Beijing:Petroleum Industry Press:1-694(in Chinese).
Liu Funing.1994.An approach to reconstruction of paleosedimentary thickness and paleo-formation pressure in abnormal high pressure region[J].Oil&Gas Geology,15(2):180-185(in Chinese).
Liao Lingling,Wang Yunpeng.2015.Retrieving paleo-pressure of the Upper Paleozoic fluid of the Ordos basin using inclusion PVTx modeling and Petro Mod basin simulation system[J].Bulletin of Mineralogy,Petrology and Geochemistry,34(5):955-959(in Chinese with English abstract).
Li Xingwei.2015.Numerical simulations of the burial&thermal histories for Daqing placanticline in north Songliao basin[J].Petroleum Geology and Oilfield Development in Daqing,34(1):46-50(in Chinese with English abstract).
Liu Bo,Wang Fan,Ran Qingchang,Li Mei,Dai Chunlei.2014.Characteristics of shale reservoir of the first member of Qingshankou Formation in northern Songliao basin[J].Lithologic Reservoirs,26(5):64-68(in Chinese with English abstract).
Li Mingcheng,Shan Xiuqin,Ma Chenghua,Hu Guoyi.2005.Approach to hydrocarbon accumulation period[J].Xinjian Petroleum Geology,26(5):587-592(in Chinese with English abstract).
Li Lei,Zuo Yinhui,Tang Shuheng,Zhang Songhang.2016.Cenozoic thermal history of the Dongpu sag,Bohai Bay basin[J].Geology and Exploration,52(3):594-600(in Chinese with English abstract).
Li Zhi'an.1995.Evolutionary features of mantle heat flux in Songliao basin[J].Geotectonica et Metallogenia,2(2):104-112(in Chinese).
Ren Zhanli.1992.Advances on thermal histories of sedimentary basins[J].Advance in Earth Sciences,7(3):43-48(in Chinese).
Ren Zhanli.1993.Research on tectonic-thermal evolution history in sedimentary basins of north China[M].Beijing:Petroleum Industry Press:1-100(in Chinese).
Shi Lizhi,Wang Zhuozhuo,Zhang Ge,Zhang Yongsheng,Xing Enyuan.2015.Distribution and formation of tight oil in Qijia area,Songliao basin,NE China[J].Petroleum Exploration and Development,42(1):44-50(in Chinese with English abstract).
Shi Lizhi,Wu Heyong,Lin Tiefeng,Wu Haibo,Wang Shibo,Wang Zhuozhuo.2007.Characteristics of hydrocarbon migration in Fuyang oil layer in Daqing placanticline and its western area in Songliao basin[J].Acta Petrolei Sinica,28(6):173-187(in Chinese with English abstract).
Shi Zhongsheng,Wang Tianqi,Wang Jiangong,Pan Shuxin,Yang Rongjun,Wang Ge.2012.Application of seismic sedimentology to sand body identification under different geological settings:A case study from the western slope and placanticline of Songliao basin[J].Lithologic Reservoirs,24(3):64-68(in Chinese with English abstract).
Sun Yu,Dong Yiming,Wang Jiping,Ma Shizhong,Yu Liming,Yan Baiquan.2016.Distribution patterns of single sand body in Fuyu oil layer in the northern Honggang area,Songliao basin[J].Lithologic Reservoirs,28(4):9-15(in Chinese with English abstract).
Shen Jianian,Wang Qinghong,He Jianglin.2008.Estimation of the ancient lake temperature and paleoclimate of the Cretaceous period in the Songliao basin[J].Journal of Jilin University(Earth Science Edition),25(2):257-265(in Chinese with English abstract).
Wang Zhiwu,Yang Jiliang,Gao Ruiqi.1993.Petroleum geology of China:Volume 2[M].Beijing:Petroleum Industry Press:79-177(in Chinese).
Wu Qianfan,Xie Yizhen.1985.Geothermal heat flow in the Songliao basin[J].Seismology and Geology,7(2):59-64(in Chinese).
Xin Rencheng,Cai Xiyuan.2004.Controls of buried history on oil accumulation processes in Daqing placanticline of northern Songliao basin[J].Earth Science-Journal of China University of Geosciences,29(4):457-460(in Chinese with English abstract).
Yang Wanli,Gao Ruiqi,Guo Qingfu,Iiu Yaoguang.1985.The continental oil generation,migration and accumulation in Songliao basin[M].Harbin:Scientific and Technical Press of Heilongjiang Province:1-347(in Chinese).
Yu Wenqing,Sun Xi,Yu Enjun,Qu Xujun.1999.Stratigraphic division of Cretaceous strata in Songliao basin[J].Uranium Geology,15(5):257-265(in Chinese)
Zhao Jingzhou.2002.Geochronology of petroleum accumulation:New advances and the future trend[J].Advance in Earth Sciences,17(3)378-384(in Chinese with English abstract).
Zhang Qingchun,Shi Guangren,Tian Zaiyi.2001.Present developing situation and future prospects of basin simulation technology[J].Petroleum Geology&Experiment,23(3):312-316(in Chinese with English abstract).
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