马东油田沙一下亚段板2、板3油组高分辨率层序地层学研究
|
摘要
马东油田为北大港油田港东开发区深层油田,目前已处在产量下降阶段。根据研究区地震、测井和岩心资料,应用高分辨率层序地层学原理,对区内板2、板3油组地层进行了多级次基准面旋回的识别和对比,将其分为1个长期基准面旋回、2个中期基准面旋回和10个短期基准面旋回;分析了基准面旋回对沉积特征、储层物性的控制作用,基准面下降后期、上升早期容易发育良好储层;基准面下降早期、上升后期,储层物性差。
As a deep oilfield,Madong Oilfield belonging to Beidagang Oilfield is at the stage of descending.On the foundation of the Seismic data,logging data and core material,the authors identified and compared base level cycles for layer BⅡ and BⅢ according to the principle of high-resolution sequence stratigraphy.Higher baselevel cycles were recognized as an long baselevel cycle,two intermediate baselevel cycles and 10 short baselevel cycles.It was analyzed that the baselevel cycles could control the sedimentary characteristics and the reservoir properties.The sand body descending at the late stage of baselevel-dropping and early stage of baselevel-rising often has well properties.While the sand body descending at the early stage of baselevel-dropping and late stage of baselevel-rising usually has bad properties.
As a deep oilfield,Madong Oilfield belonging to Beidagang Oilfield is at the stage of descending.On the foundation of the Seismic data,logging data and core material,the authors identified and compared base level cycles for layer BⅡ and BⅢ according to the principle of high-resolution sequence stratigraphy.Higher baselevel cycles were recognized as an long baselevel cycle,two intermediate baselevel cycles and 10 short baselevel cycles.It was analyzed that the baselevel cycles could control the sedimentary characteristics and the reservoir properties.The sand body descending at the late stage of baselevel-dropping and early stage of baselevel-rising often has well properties.While the sand body descending at the early stage of baselevel-dropping and late stage of baselevel-rising usually has bad properties.
引文
[1]孟万斌.从层序地层学到高分辨率层序地层学[J].成都理工学院学报,2002,29(4):380-385.
[2]纪友亮.层序地层学[M].上海:同济大学出版社,2005:3-11.
[3]李希宗.层序地层学问题讨论[J].中国海上油气(地质),1994,8(3):179-182.
[4]杨国臣,于炳松.层序地层学的发展现状及其学科地位与研究前沿[J].石油地质与工程,2009,23(2):1-5.
[5]刘招君,程日辉,易海永.层序地层学的概念、进展与争论[J].世界地质,1994,13(3):56-68.
[6]李劲松,郑晓东,高志勇,等.高分辨率层序地层学在提高储集层预测精度中的应用[J].石油勘探与开发,2009,36(4):448-455.
[7]王嗣敏,刘招君.高分辨率层序地层学在陆相地层研究中若干问题的讨论[J].地层学杂志,2004,28(2):179-184.
[8]邓宏文.美国层序地层研究中的新学派-高分辨率层序地层学[J].石油与天然气地质,1995,16(2):89-97.
[9]胡孝林,黎明碧,郑荣才.高分辨率层序地层学理论探析[J].中国海上油气(地质),1999,13(2):73-78.
[10]钟建华,孙正贵,禚元杰,等.高分辨率层序地层学的应用——以河125断层区沙三中亚段为例[J].地质找矿论丛,2009,24(3):243-248.
[11]刘学锋,卢顺容.黄骅拗陷构造运动程式探讨[J].西南石油学院学报,1995,17(2):8-14.
[12]王光奇,漆家福,岳云福.歧口凹陷及周缘新生代构造的成因和演化[J].地质科学,2003,38(2):230-240.
[13]严德天,王华,王家豪,等.黄骅坳陷沙河街组层序地层样式及隐蔽圈闭预测[J].中国矿业大学学报,2008,37(1):30-37.
[14]朱筱敏,董艳蕾,郭长敏,等.歧口凹陷沙河街组一段层序格架和储层质量分析[J].沉积学报,2007,25(6):934-940.
[15]尹伟,林双运,赵郁文,等.马东东地区深部储层物性影响因素分析[J].中国海上油气(地质),2003,17(2):104-107.
[16]谭守强,刘震,孙晓明,等.歧口凹陷马东东地区沙一段油气成藏期次[J].油气地质与采收率,2004,11(5):24-26.
[17]程立华,吴胜和,宋春刚,等.黄骅坳陷马东地区古近系重力流水道相储层特征研究[J].西安石油大学学报,2008,23(6):33-41.
[18]张晓华,张金亮.高分辨率层序地层学在濮城油田西区沙一上亚段2+3砂组末端扇沉积体系中的应用[J].地层学杂志,2008,32(4):426-438.
[19]ZHANG Jinliang,JIANG Zhiqiang,LI Deyong,et al.Sequencestratigraphic analysis of the first layer,Upper second Sub-mem-ber Shahejie Formation in Pucheng Oilfield[J].Journal of EarthScience,2009,20(6):932-940.
[20]邓宏文,王洪亮,李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2):90-95.
[21]郝素凤,马立祥.高分辨率层序地层学在油田上的应用[J].沉积与特提斯地质,2002,22(4):102-106.
[22]邓宏文,王洪亮,祝永军,等.高分辨率层序地层学-原理及应用[M].北京:地质出版社,2002.
[23]邓宏文,王洪亮,李熙喆.层序地层地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177-184.
[24]孙宝玲,唐民安.基准面旋回识别的原理与方法[J].资源环境与工程,2008,22(4):457-467.
[25]赵志魁,张金亮,赵占银,等.松辽盆地南部坳陷湖盆沉积相和储层研究[M].北京:石油工业出版社,2009:27-52.
[26]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375.
[27]何玉平,刘招君,杜江峰.高分辨率层序地层学基准面旋回识别[J].世界地质,2003,22(1):21-25.
[28]孙海雷,柳成志,李明辉,等.高分辨率层序地层学在辽河油田大民屯凹陷油田精细开发中的应用[J].现代地质,2009,23(5):981-986.
[29]常德双,卢刚臣,孔凡东,等.大港探区湖泊浅水滩、坝油气藏勘探浅析[J].中国石油勘探,2004,2:26-32.
[30]朱筱敏.层序地层学[M].东营:石油大学出版社,2000.
[2]纪友亮.层序地层学[M].上海:同济大学出版社,2005:3-11.
[3]李希宗.层序地层学问题讨论[J].中国海上油气(地质),1994,8(3):179-182.
[4]杨国臣,于炳松.层序地层学的发展现状及其学科地位与研究前沿[J].石油地质与工程,2009,23(2):1-5.
[5]刘招君,程日辉,易海永.层序地层学的概念、进展与争论[J].世界地质,1994,13(3):56-68.
[6]李劲松,郑晓东,高志勇,等.高分辨率层序地层学在提高储集层预测精度中的应用[J].石油勘探与开发,2009,36(4):448-455.
[7]王嗣敏,刘招君.高分辨率层序地层学在陆相地层研究中若干问题的讨论[J].地层学杂志,2004,28(2):179-184.
[8]邓宏文.美国层序地层研究中的新学派-高分辨率层序地层学[J].石油与天然气地质,1995,16(2):89-97.
[9]胡孝林,黎明碧,郑荣才.高分辨率层序地层学理论探析[J].中国海上油气(地质),1999,13(2):73-78.
[10]钟建华,孙正贵,禚元杰,等.高分辨率层序地层学的应用——以河125断层区沙三中亚段为例[J].地质找矿论丛,2009,24(3):243-248.
[11]刘学锋,卢顺容.黄骅拗陷构造运动程式探讨[J].西南石油学院学报,1995,17(2):8-14.
[12]王光奇,漆家福,岳云福.歧口凹陷及周缘新生代构造的成因和演化[J].地质科学,2003,38(2):230-240.
[13]严德天,王华,王家豪,等.黄骅坳陷沙河街组层序地层样式及隐蔽圈闭预测[J].中国矿业大学学报,2008,37(1):30-37.
[14]朱筱敏,董艳蕾,郭长敏,等.歧口凹陷沙河街组一段层序格架和储层质量分析[J].沉积学报,2007,25(6):934-940.
[15]尹伟,林双运,赵郁文,等.马东东地区深部储层物性影响因素分析[J].中国海上油气(地质),2003,17(2):104-107.
[16]谭守强,刘震,孙晓明,等.歧口凹陷马东东地区沙一段油气成藏期次[J].油气地质与采收率,2004,11(5):24-26.
[17]程立华,吴胜和,宋春刚,等.黄骅坳陷马东地区古近系重力流水道相储层特征研究[J].西安石油大学学报,2008,23(6):33-41.
[18]张晓华,张金亮.高分辨率层序地层学在濮城油田西区沙一上亚段2+3砂组末端扇沉积体系中的应用[J].地层学杂志,2008,32(4):426-438.
[19]ZHANG Jinliang,JIANG Zhiqiang,LI Deyong,et al.Sequencestratigraphic analysis of the first layer,Upper second Sub-mem-ber Shahejie Formation in Pucheng Oilfield[J].Journal of EarthScience,2009,20(6):932-940.
[20]邓宏文,王洪亮,李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2):90-95.
[21]郝素凤,马立祥.高分辨率层序地层学在油田上的应用[J].沉积与特提斯地质,2002,22(4):102-106.
[22]邓宏文,王洪亮,祝永军,等.高分辨率层序地层学-原理及应用[M].北京:地质出版社,2002.
[23]邓宏文,王洪亮,李熙喆.层序地层地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177-184.
[24]孙宝玲,唐民安.基准面旋回识别的原理与方法[J].资源环境与工程,2008,22(4):457-467.
[25]赵志魁,张金亮,赵占银,等.松辽盆地南部坳陷湖盆沉积相和储层研究[M].北京:石油工业出版社,2009:27-52.
[26]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375.
[27]何玉平,刘招君,杜江峰.高分辨率层序地层学基准面旋回识别[J].世界地质,2003,22(1):21-25.
[28]孙海雷,柳成志,李明辉,等.高分辨率层序地层学在辽河油田大民屯凹陷油田精细开发中的应用[J].现代地质,2009,23(5):981-986.
[29]常德双,卢刚臣,孔凡东,等.大港探区湖泊浅水滩、坝油气藏勘探浅析[J].中国石油勘探,2004,2:26-32.
[30]朱筱敏.层序地层学[M].东营:石油大学出版社,2000.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心