源断砂空间匹配输导油气有效性研究
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摘要
为了更好地指导含油气盆地下生上储式生储盖组合油气勘探,在源岩、油源断裂和砂体空间匹配输导油气有效性及其影响因素研究的基础上,通过确定优质源岩分布和油源断裂输导脊分布,确定源断空间匹配油气充注有利部位,结合侧向分流运移砂体空间分布,提出判断源断砂空间匹配输导油气有效性的方法.研究结果表明:留楚地区北部和中部东营组二段下亚段、中亚段和上亚段分别有24,24和16个源断空间匹配油气充注有利部位与侧向分流运移砂体距离小于0,源断砂空间匹配输导油气有效性判断为好,有利于油气向东营组二段侧向分流运移,油气富集;东营组三段下亚段、中亚段和上亚段分别有21,25和22个源断空间匹配油气充注有利部位与侧向分流运移砂体距离小于0,源断砂空间匹配输导油气有效性判断为好,有利于油气向东营组三段侧向分流运移,油气富集.西部边部、中部和东部东营组三段下亚段、中亚段和上亚段分别有13,7和14个源断空间匹配油气充注有利部位与侧向分流运移砂体距离在0～1.2 km之间,源断砂空间匹配输导油气有效性判断为较差,不利于油气向东营组三段侧向分流运移,无油气富集;东营组二段下亚段、中亚段和上亚段分别有7,10和18个源断空间匹配油气充注有利部位与侧向分流运移砂体距离在0～1.2 km之间,源断砂空间匹配输导油气有效性判断为较差,不利于油气向东营组二段侧向分流运移,无油气富集.东南部东营组二段和三段源断空间匹配油气充注有利部位与侧向分流运移砂体距离大于1.2 km,源断砂空间匹配输导油气有效性判断为更差,油气无法向东营组二段和三段侧向分流运移,无油气富集.
To better guide the exploration of oil and gas in lower generation-upper accumulation source rock-reservoir-cap rocks in oil and gas bearing basins, an effective method for judging the effectiveness of transporting oil and gas of source-fault-sandstone space matching was put forward. The method was derived based on influence factors and the effectiveness of transporting oil and gas of source-fault-sandstone space matching, by determining the favorable location for hydrocarbon charging of source-fault space matching through determining the maturation zone of source rock and the distribution of transporting ridge, and combined with the space distribution of lateral distributary movement sandstone. The results show that in the north and the middle of Liuchu area, there are 24, 24 and 16 favorable locations for hydrocarbon charging of source-fault space matching in Ed2~1, Ed2~2 and Ed2~3 respectively. Their distance to the lateral distributary movement sandstone is less than 0, and the effectiveness of transporting oil and gas of space matching of source-fault-sandstone is perfect, which is favorable for lateral migration and accumulation of oil and gas to the Ed2. There are 21, 25 and 22 favorable locations for hydrocarbon charging of source-fault space matching in Ed3~1, Ed3~2 and Ed3~3 respectively, and their distance to the lateral distributary movement sandstone is less than 0, and the effectiveness of transporting oil and gas of source-fault-sandstone space matching is perfect, which is favorable for lateral migration and accumulation of oil and gas to the Ed3. In the edge of west, central and the edge of east, there are 13, 7 and 14 favorable locations for hydrocarbon charging of source-fault space matching in Ed3~1, Ed3~2 and Ed3~3 respectively, and their distance to the lateral distributary movement sandstone is 0—1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is bad, which is unfavorable for lateral migration and accumulation of oil and gas to the Ed3. There are 7, 10 and 18 favorable locations for hydrocarbon charging of source-fault space matching in Ed2~1, Ed2~2 and Ed2~3 respectively, and their distance to the lateral distributary movement sandstone is 0—1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is bad, which is unfavorable for lateral migration and accumulation of oil and gas to the Ed2. In the southeast, the distance between the unfavorable locations for hydrocarbon charging of source-fault space matching in Ed2 and Ed3 and the lateral distributary movement sandstone is greater than 1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is worse, as a result, the oil and gas cannot migrate laterally to Ed2 and Ed3 and there is no accumulation of oil and gas.
To better guide the exploration of oil and gas in lower generation-upper accumulation source rock-reservoir-cap rocks in oil and gas bearing basins, an effective method for judging the effectiveness of transporting oil and gas of source-fault-sandstone space matching was put forward. The method was derived based on influence factors and the effectiveness of transporting oil and gas of source-fault-sandstone space matching, by determining the favorable location for hydrocarbon charging of source-fault space matching through determining the maturation zone of source rock and the distribution of transporting ridge, and combined with the space distribution of lateral distributary movement sandstone. The results show that in the north and the middle of Liuchu area, there are 24, 24 and 16 favorable locations for hydrocarbon charging of source-fault space matching in Ed2~1, Ed2~2 and Ed2~3 respectively. Their distance to the lateral distributary movement sandstone is less than 0, and the effectiveness of transporting oil and gas of space matching of source-fault-sandstone is perfect, which is favorable for lateral migration and accumulation of oil and gas to the Ed2. There are 21, 25 and 22 favorable locations for hydrocarbon charging of source-fault space matching in Ed3~1, Ed3~2 and Ed3~3 respectively, and their distance to the lateral distributary movement sandstone is less than 0, and the effectiveness of transporting oil and gas of source-fault-sandstone space matching is perfect, which is favorable for lateral migration and accumulation of oil and gas to the Ed3. In the edge of west, central and the edge of east, there are 13, 7 and 14 favorable locations for hydrocarbon charging of source-fault space matching in Ed3~1, Ed3~2 and Ed3~3 respectively, and their distance to the lateral distributary movement sandstone is 0—1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is bad, which is unfavorable for lateral migration and accumulation of oil and gas to the Ed3. There are 7, 10 and 18 favorable locations for hydrocarbon charging of source-fault space matching in Ed2~1, Ed2~2 and Ed2~3 respectively, and their distance to the lateral distributary movement sandstone is 0—1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is bad, which is unfavorable for lateral migration and accumulation of oil and gas to the Ed2. In the southeast, the distance between the unfavorable locations for hydrocarbon charging of source-fault space matching in Ed2 and Ed3 and the lateral distributary movement sandstone is greater than 1.2 km. The effectiveness of transporting oil and gas of source-fault-sandstone space matching is worse, as a result, the oil and gas cannot migrate laterally to Ed2 and Ed3 and there is no accumulation of oil and gas.
引文
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[3] 王金生,付广,刘洪霞,等.从源盖断时空匹配关系剖析乌尔逊凹陷南二段油气前景[J].大庆石油地质与开发,2005,24(4):1-3.WANG Jinsheng,FU Guang,LIU Hongxia,et al.Analysis of oil and gas prospecting of K1n2 in Wuerxun depression from time-space matching relation among source rock,cap rock and faults[J].Petroleum Geology & Oilfield Development in Daqing,2005,24(4):1-3.
[4] 付广,吕延防,付晓飞,等.断陷盆地源盖断时空匹配关系对油气成藏的控制作用[J].油气地质与采收率,2004,11(5):17-20.FU Guang,LYU Yanfang,FU Xiaofei,et al.Time-space matching relation of source rock,caprock and faults and its controlling effect on oil and gas reservoir forming in fault basin[J].Petroleum Geology and Recovery Efficiency,2004,11(5):17-20.
[5] 王阳洋,陈践发,庞雄奇,等.塔中地区奥陶系油气充注特征及运移方向[J].石油学报,2018,39(1):54-68.WANG Yangyang,CHEN Jianfa,PANG Xiongqi,et al.Ordovician hydrocarbon charging characteristics and migration direction in Tazhong area[J].Acta Petrolei Sinica,2018,39(1):54-68.
[6] 吴文祥,张海翔,李占东,等.层序地层地球化学方法在烃源岩评价中的应用:以海拉尔盆地贝尔凹陷为例[J].石油与天然气地质,2015,34(4):701-710.WU Wenxiang,ZHANG Haixiang,LI Zhandong,et al.Sequence stratigraphic geochemistry and its application in evaluation of source rocks:Taking Beier sag of Hailar basin as an example[J].Oil & Gas Geology,2015,34(4):701-710.
[7] 卢双舫,马延伶,曹瑞成,等.优质烃源岩评价标准及其应用:以海拉尔盆地乌尔逊凹陷为例[J].地球科学(中国地质大学学报),2012,37(3):535-544.LU Shuangfang,MA Yanling,CAO Ruicheng,et al.Evaluation criteria of high-quality source rocks and its applications:Taking the Wuerxun sag in Hailaer basin as an example[J].Earth Science,2012,37(3):535-544.
[8] 侯读杰,张善文,肖建新,等.济阳坳陷优质烃源岩特征与隐蔽油气藏的关系分析[J].地学前缘,2008,15(2):137-146.HOU Doujie,ZHANG Shanwen,XIAO Jianxin,et al.The excellent source rocks and accumulation of stratigraphic and lithologic traps in the Jiyang depression,Bohai bay basin,China[J].Earth Science Frontiers,2008,15(2):137-146.
[9] 谢昭涵,孙永河,闫玉民,等.尼日尔三角洲E背斜顶部断裂演化机制及封闭性[J].石油与天然气地质,2017,38(5):973-982.XIE Zhaohan,SUN Yonghe,YAN Yumin,et al.Structural evolution mechanism and sealing of faults on the crest of anticline E in Niger Delta[J].Oil & Gas Geology,2017,38(5):973-982.
[10] 童亨茂,赵宝银,曹哲,等.渤海湾盆地南堡凹陷断裂系统成因的构造解析[J].地质学报,2013,87(11):1647-1661.TONG Hengmao,ZHAO Baoyin,CAO Zhe,et al.Structural analysis of faulting system origin in the Nanpu sag,Bohai bay basin[J].Acta Geologica Sinica,2013,87(11):1647-1661.
[11] 何书,杨桥,漆家福,等.黄骅坳陷中区新生代断裂系统及其成因分析[J].地质科学,2008,43(3):533-545.HE Shu,YANG Qiao,QI Jiafu,et al.Cenozoic fault systems and their genetic analysis in central area of the Huanghua depression[J].Chinese Journal of Geology,2008,43(3):533-545.
[12] 陈凯,漆家福,刘震,等.渤海海域渤东地区新生代断裂特征及对油气的控制[J].地质科技情报,2012,31(1):63-71.CHEN Kai,QI Jiafu,LIU Zhen,et al.Characteristics of cenozoic fault systems and dominating action on hydrocarbon accumulation in eastern Bohai sea area[J].Geological Science and Technology Information,2012,31(1):63-71.
[13] 吕延防,韦丹宁,孙永河,等.南堡凹陷断层对中、上部含油组合油气成藏的控制作用[J].吉林大学学报(地球科学版),2015,45(4):971-982.LYU Yanfang,WEI Danning,SUN Yonghe,et al.Control action of faults on hydrocarbon migration and accumulation in the middle and upper oil-bearing group in Nanpu sag[J].Journal of Jilin University (Earth Science Edition),2015,45(4):971-982.
[14] 付广,王浩然.不同时期油源断裂输导油气有利部位确定方法及其应用[J].石油学报,2018,39(2):180-188.FU Guang,WANG Haoran.Determination method and its application of favorable positions for hydrocarbon transport in oil-source fault during different periods[J].Acta Petrolei Sinica,2018,39(2):180-188.
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