松辽盆地泰康隆起带青二、三段储层流体包裹体特征与成藏期次
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摘要
基于流体包裹体测试资料,应用PetroMod-1D软件恢复泰康隆起带代表井的埋藏史、热史和生烃史,对松辽盆地泰康隆起带青二、三段储层油气成藏期次特征进行了综合分析。研究表明:泰康隆起带青二、三段砂岩储层中包含液态烃、气液烃、气态烃和含烃盐水4种包裹体,包裹体颜色主要显示为淡黄色、黄绿色、绿色、蓝白色和蓝色荧光;流体包裹体均一温度和盐度均呈现双峰特征,其中均一温度2个峰值分别为80～90℃和100～110℃,盐度2个峰值分别为2%～4%和6%～8%,表明储层中主要有2期油气充注;第1期包裹体形成于嫩江组沉积末,该期圈闭初具雏形,齐家—古龙凹陷青山口组烃源岩进入排烃门限,泰康隆起带青二、三段储层充注少量低成熟的气态烃和液态烃;第2期包裹体形成于明水组沉积末,圈闭已定型,齐家—古龙凹陷青山口组烃源岩达到排烃高峰,且与区域性构造运动时期相对应,是泰康隆起带青二、三段储层的关键油气成藏期。该研究成果为泰康隆起带油气成藏地质时期研究和勘探目标优选提供了依据。
Based on the test date of the fluid inclusion, the burial, thermal and hydrocarbon-generated histories were reconstructed for the representative wells in Taikang Uplift Belt with the help of Software PetroMod-1 D, the comprehensive analysis was conducted for the characteristics of the hydrocarbon accumulation period in Member Qing2-3 reservoirs of Taikang Uplift Belt of Songliao Basin. The study shows that four types of the fluid inclusions occur in Member Qing2-3 sandstone reservoirs, including the liquid hydrocarbon, gas-liquid hydrocarbon, gas hydrocarbon and hydrocarbon-containing brine. The inclusions are mainly displayed in pale yellow, yellow green, green, blue white and blue fluorescence; the homogenized temperature and salinity of the fluid inclusions appear to be bimodal, for the former, there are two major peak values at 80-90 ℃ and 100-110 ℃ and for the later here are two major peak values at 2%-4% and 6%-8%,these indicate that there are two main hydrocarbon charged and filled stages in the reservoirs; the first-stage inclusion was formed at the end of Nenjiang Formation sedimentation, the trap just took shape, the source rocks of Qingshankou Formation in Qijia-Gulong Sag entered the hydrocarbon-expelled threshold, Member Qing2-3 sandstone reservoirs in Taikang Uplift Belt was filled with a small amount of low-maturity gaseous hydrocarbon and liquid hydrocarbon;the second-stage inclusion was formed and sedimentated in the end of Mingshui Formation and moreover the traps were shaped with the regional tectonic movement and the source rocks of Qingshankou Formation in Qijia-Gulong Sag entered the peak of the hydrocarbon expulsion, so it has been the key period of the hydrocarbon accumulation in Member Qing2-3 reservoirs. The study results have provided the evidences for the researches on the geological period of the petroleum accumulation and the optimization of the exploration target in Taikang Uplift Belt.
Based on the test date of the fluid inclusion, the burial, thermal and hydrocarbon-generated histories were reconstructed for the representative wells in Taikang Uplift Belt with the help of Software PetroMod-1 D, the comprehensive analysis was conducted for the characteristics of the hydrocarbon accumulation period in Member Qing2-3 reservoirs of Taikang Uplift Belt of Songliao Basin. The study shows that four types of the fluid inclusions occur in Member Qing2-3 sandstone reservoirs, including the liquid hydrocarbon, gas-liquid hydrocarbon, gas hydrocarbon and hydrocarbon-containing brine. The inclusions are mainly displayed in pale yellow, yellow green, green, blue white and blue fluorescence; the homogenized temperature and salinity of the fluid inclusions appear to be bimodal, for the former, there are two major peak values at 80-90 ℃ and 100-110 ℃ and for the later here are two major peak values at 2%-4% and 6%-8%,these indicate that there are two main hydrocarbon charged and filled stages in the reservoirs; the first-stage inclusion was formed at the end of Nenjiang Formation sedimentation, the trap just took shape, the source rocks of Qingshankou Formation in Qijia-Gulong Sag entered the hydrocarbon-expelled threshold, Member Qing2-3 sandstone reservoirs in Taikang Uplift Belt was filled with a small amount of low-maturity gaseous hydrocarbon and liquid hydrocarbon;the second-stage inclusion was formed and sedimentated in the end of Mingshui Formation and moreover the traps were shaped with the regional tectonic movement and the source rocks of Qingshankou Formation in Qijia-Gulong Sag entered the peak of the hydrocarbon expulsion, so it has been the key period of the hydrocarbon accumulation in Member Qing2-3 reservoirs. The study results have provided the evidences for the researches on the geological period of the petroleum accumulation and the optimization of the exploration target in Taikang Uplift Belt.
引文
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[2]王传远, 段毅, 杜建国,等. 鄂尔多斯盆地长9油层组流体包裹体特征与油气成藏期次分析[J].地质科技情报, 2009, 28(4):47-50.WANG Chanyuan, DUAN Yi, DU Jianguo, et al. Hydrocarbon migration stages in Chang 9 Formation in Ordos Basin by fluid inclusion analysis[J]. Geological Science & Technology Information, 2009, 28(4):47-50.
[3]赵靖舟. 塔里木盆地烃类流体包裹体与成藏年代分析[J].石油勘探与开发, 2002, 29(4):21-25.ZHOU Jingzhou. Geochronology of hydrocarbon accumulation in the Tarim Basin:Evidence from fluid inclusion[J].Petroleum Exploration & Development, 2002, 29(4):21-25.
[4]KARLSEN D A, NEDKVITNE T, LARTER S R, et al. Hydrocarbon composition of authogenic inclusions: Application to elucidation of petroleum reservoir filling history[J].Geochimica et Cosmochimica Acta, 1993, 57(15):3641-3659.
[5]高勇, 牟智全, 王永凯,等. 流体包裹体在油气成藏研究中的应用[J].特种油气藏, 2012, 19(4):37-41.GAO Yong, MU Zhiquan,WANG Yongkai, et al. Application of fluid inclusion in hydrocarbon accumulation study[J].Special Oil & Gas Reservoirs, 2012, 19(4):37-41.
[6]刘德良, 陶士振, 张宝民. 包裹体在确定成藏年代中的应用及应注意的问题[J].天然气地球科学, 2005, 16(1):16-19.LIU Deliang,TAO Shizhen, ZHANG Baomin. Application and questions about ascertaining oil-gas pools age with inclusion[J].Natural Gas Geoscience, 2005, 16(1):16-19.
[7]许浩, 汤达祯, 魏国齐,等. 川西地区须二段油气充注历史的流体包裹体分析[J].天然气地球科学, 2005, 16(5):571-574.XU Hao,TANG Dazhen, WEI Guoqi, et al. Study on the hydrocarbon charge history in the 2nd Member of Xujiahe Formation of West Sichuan by evidence from fluid inclusions[J].Natural Gas Geoscience, 2005, 16(5):571-574.
[8]赵鸿皓, 蒋有录, 张惠,等. 长岭断陷龙凤山次凹下白垩统油气成藏期[J].大庆石油地质与开发, 2017, 36(6):58-63. ZHAO Honghao,JIANG Youlu,ZHANG Hui, et al. Accumulation stages of lower Cretaceous hydrocarbon in Longfengshan Subsag of Changling Fault Depression[J].Petroleum Geology & Oilfield Development in Daqing, 2017, 36(6):58-63.
[9]李美俊, 王铁冠, 刘菊,等. 由流体包裹体均一温度和埋藏史确定油气成藏时间的几个问题:以北部湾盆地福山凹陷为例[J].石油与天然气地质, 2007, 28(2):151-158.LI Meijun, WANG Tieguan, LIU Ju, et al. A discussion on hydrocarbon accumulation dating determined by homogenization temperature and burial history of fluid inclusions: An example from the Fushan Depression, Beibuwan Basin[J].Oil & Gas Geology, 2007, 28(2):151-158.
[10]张君峰, 喻廷旭, 许浩,等. 柴达木盆地南翼山油田新近系油藏包裹体与成藏特征[J].大庆石油地质与开发, 2015, 34(5):32-37.ZHANG Junfeng,YU Tingxu,XU Hao,et al. Inclusions and reservoir-forming characteristics of the Neogene reservoirs in Nanyishan Oilfield of Qaidam Basin[J].Petroleum Geology & Oilfield Development in Daqing, 2015, 34(5):32-37.
[11]XU Hao,TANG Dazhen.Application of fluid inclusion technology to the study of hydrocarbon charge history in Upper Triassic reservoir of Chuanxi foreland Basin,China[J].Advanced Materials Research, 2011, 339(1):517-520.
[12]韩强, 李宗杰, 杨子川,等. 塔里木盆地三道桥地区油气成藏特征[J].油气地质与采收率, 2015, 22(6):14-20.HAN Qiang,LI Zongjie, YANG Zichuan, et al.Characteristics of hydrocarbon accumulation in the Sandaoqiao area of Tarim Basin[J].Petroleum Geology & Recovery Efficiency, 2015, 22(6):14-20.
[13]张亮. 潜江凹陷钟市地区油气成藏特征及成藏模式[J].特种油气藏, 2016, 23(4):69-72.ZHANG Liang. Hydrocarbon accumulation characteristics and accumulation model in Zhongshi area, Qianjiang Depression[J].Special Oil & Gas Reservoirs, 2016, 23(4):69-72.
[14]BURRUSS R C. Practical aspects of fluorescence microscopy of petroleum fluid inclusions[J].Society of Economic Paleontologists & Mineralogists, 1991, 25(1):1-7.
[15]张文忠, 郭彦如, 汤达祯,等. 苏里格气田上古生界储层流体包裹体特征及成藏期次划分[J].石油学报, 2009, 30(5):685-691.ZHANG Wenzhong,GUO Yanru, TANG Dazhen, et al. Characteristics of fluid inclusions and determination of gas accumulation period in the Upper Paleozoic reservoirs of Sulige Gas Field[J].Acta Petrol Sin, 2009, 30(5):685-691.
[16]侯启军, 冯子辉, 邹玉良. 松辽盆地齐家—古龙凹陷油气成藏期次研究[J].石油实验地质, 2005, 27(4):390-394.HOU Qijun, FENG Zihui, ZOU Yuliang.Study on the pool-forming periods of oil and gas in Qijia-Gulong Sag in Songliao Basin[J].Petroleum Geology & Experiment, 2005, 27(4):390-394.
[17]周庆华, 吕延防, 付广,等. 松辽盆地北部西斜坡油气成藏模式和主控因素[J].天然气地球科学, 2006, 17(6):765-769.ZHOU Qinghua,Lü Yanfang, FU Guang, et al. The pool-forming pattern and main control factors in West Slope of the north of Songliao Basin[J].Natural Gas Geoscience, 2006, 17(6):765-769.
[18]斯尚华, 赵靖舟, 蒙启安,等. 松辽盆地齐家地区高台子致密油层包裹体古流体压力特征及其地质意义[J].地质力学学报, 2018, 24(1):51-59.SI Shanghua,ZHAO Jingzhou,MENG Qi’an,et al.The fluid inclusion paleo pressure characteristics and geological implications of Gaotaizi tight reservoir in Qijia area of Songliao Basin[J].Journal of Geomechanics, 2018, 24(1):51-59.
[19]梁江平. 松辽盆地北部西斜坡区萨二、三油层油气藏形成机理研究[D].大庆:大庆石油学院, 2007.LIANG Jiangping.Research on formation mechanism of oil-gas reservoirs of S2+3 oil layer in West Slope region,North Songliao Basin[D].Daqing:Daqing Petroleum Institute, 2007.
[20]樊金生.松辽盆地北部西斜坡萨尔图油层层序、沉积相研究及地层—岩性圈闭预测[D].大庆:大庆石油学院, 2006.FAN Jinsheng.The research of the saertu oil-bearing sequence sedimentary facies and the prediction of the formation-lithologic trap of the west slop on the north of the Songliao Basin[D].Daqing:Petroleum Institute, 2007.
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