冀中坳陷八里庄—薛庄潜山带构造演化与油气成藏
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摘要
八里庄—薛庄潜山带是冀中坳陷内最为典型的断块型潜山带。为进一步了解该潜山带构造特征及其成藏条件,利用地震、钻井等资料,分析了其形成演化过程。研究认为,八里庄—薛庄潜山带的形成演化过程经历了中新元古代至古生代潜山的物质基础发育期、中生代潜山的初始形成期、早第三纪潜山的主要定型期以及晚第三纪至第四纪潜山的深埋期。构造演化事件影响和控制了该潜山带的油源条件、储集条件、盖层条件、输导条件、圈闭类型、油藏类型等,使其具有优越的油气成藏条件,是今后发现规模储量的有利区带,也是潜山勘探选区重要的评价依据。
Balizhuang-Xuezhuang buried hill belt is a typical fault-block buried hill belt in Jizhong Depression.The paper analyzes the forming and evolution process of Balizhuang-Xuezhuang buried hill belt by seismic and drilling data for the structural characteristics and reservoir-forming conditions.The results indicate that the evolution process of Balizhuang-Xuezhuang buried hill belt is divided into four phases.The first phase is the development of buried hill material from Meso-Neoproterozoic to Palaeozoic.The second phase is the forming of buried hill rudiment in Mesozoic.The third phase is the main development and formation of buried hill in Early Teriary.The last phase is the deep burial period of buried hill from Neogene to Quaternary.The tectonic events in Balizhuang-Xuezhuang area can be treated as the most important factor for evaluating hydrocarbon bearing potential in buried hills,due to their domination in oil resources,reservoir conditions,transporting conditions,trap-reservoir types in Balizhuang-Xuezhuang buried hill belt.
Balizhuang-Xuezhuang buried hill belt is a typical fault-block buried hill belt in Jizhong Depression.The paper analyzes the forming and evolution process of Balizhuang-Xuezhuang buried hill belt by seismic and drilling data for the structural characteristics and reservoir-forming conditions.The results indicate that the evolution process of Balizhuang-Xuezhuang buried hill belt is divided into four phases.The first phase is the development of buried hill material from Meso-Neoproterozoic to Palaeozoic.The second phase is the forming of buried hill rudiment in Mesozoic.The third phase is the main development and formation of buried hill in Early Teriary.The last phase is the deep burial period of buried hill from Neogene to Quaternary.The tectonic events in Balizhuang-Xuezhuang area can be treated as the most important factor for evaluating hydrocarbon bearing potential in buried hills,due to their domination in oil resources,reservoir conditions,transporting conditions,trap-reservoir types in Balizhuang-Xuezhuang buried hill belt.
引文
[1]李洪辉,邬光辉,王洪江,等.塔里木盆地和田河气田周缘构造演化、成藏与勘探领域[J].现代地质,2009,23(4):587-594.
[2]康玉柱,康志宏.塔里木盆地构造演化与油气[J].地球学报,1994,15(3/4):180-191.
[3]陆克政,漆家福,戴俊生.渤海湾新生代含油气盆地构造模式[M].北京:地质出版社,1997:1-50.
[4]Macgregor D S.Factors controlling the destruction or preservationof giant light oilfields[J].Petroleum Geoscience,1996,2:197-217.
[5]汪伟光,喻莲,宋成鹏,等.委内瑞拉马拉开波盆地构造演化对油气的控制[J].现代地质,2012,26(1):131-138.
[6]吴永平,付立新,杨池银,等.黄骅坳陷中生代构造演化对潜山油气成藏的影响[J].石油学报,2002,23(2):16-21.
[7]冯建伟,戴俊生,葛盛权.准噶尔盆地乌夏断裂带构造演化及油气聚集[J].中国石油大学学报:自然科学版,2008,32(3):23-29.
[8]Blanc J.Reservation,degradation and destruction of traped oil[M]//MagoonL B,Dow W G.The Petroleum System:fromSource to Trap.Tusler:AAPG,1994:73-89.
[9]何海清,王兆云,韩品龙.华北地区构造演化对渤海湾油气形成和分布的控制[J].地质学报,1998,72(4):313-321.
[10]邹华耀,向龙斌,梁宏斌,等.冀中坳陷潜山油气运聚动力学特征及其类型[J].地球科学:中国地质大学学报,2001,26(1):67-72.
[11]苏立萍,罗平,邹伟宏,等.冀中坳陷斜坡带奥陶系潜山油气成藏条件分析[J].大地构造与成矿学,2003,27(2):191-196.
[12]孙冬胜,刘池阳,杨明慧,等.渤海湾盆地冀中坳陷中区中新生代复合伸展构造[J].地质论评,2004,50(5):484-491.
[13]袁选俊,靳久强,孟庆仁,等.冀中坳陷杨村斜坡结构成因及油气成藏模式[J].石油学报,2004,25(4):19-22.
[14]于炳松,樊太亮.塔里木盆地寒武系—奥陶系泥质烃源岩发育的构造和沉积背景控制[J].现代地质,2008,22(4):534-539.
[15]崔军平,任战利.内蒙古海拉尔盆地乌尔逊凹陷热演化史[J].现代地质,2011,25(4):668-674.
[16]孙永河,漆家福,吕延防,等.渤中坳陷断裂构造特征及其对油气的控制[J].石油学报,2008,29(5):669-675.
[17]金涛,罗传容,吴亚军.岩溶作用对沙雅隆起奥陶系碳酸盐岩储集层的控制作用[J].沉积与特提斯地质,2001,21(1):27-32.
[18]牛玉静,康志宏,龙旭,等.塔河油田奥陶系岩溶油藏溶洞储集体成因及演化[J].现代地质,2011,25(4):650-659.
[19]林会喜.济阳坳陷桩西埕岛地区下古生界潜山储层岩溶作用[J].成都理工大学学报:自然科学版,2004,31(5):490-497.
[20]陈景山,李忠,王振宇,等.塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布[J].沉积学报,2007,25(6):858-868.
[21]杜学斌,解习农,任建业,等.济阳坳陷中生界古潜山油藏输导体系及成藏模式[J].地质科技情报,2005,24(2):22-26.
[22]孟卫工,陈振岩,李湃,等.潜山油气藏勘探理论与实践:以辽河坳陷为例[J].石油勘探与开发,2009,36(2):136-143.
[23]代寒松,赵锡奎,刘树根,等.塔里木盆地雅克拉断凸前中生界潜山构造与油气成藏[J].新疆石油地质,2009,30(1):17-20.
[24]付兆辉,高喜龙,陆友明,等.渤海湾盆地垦东凸起构造特征与油气聚集[J].现代地质,2008,22(4):619-627.
[25]于福生,阿木古冷,杨光达,等.准噶尔盆地车—莫古隆起的构造演化特征及其成因模拟[J].地球学报,2008,29(1):39-44.
[26]杨明慧.渤海湾盆地变换构造特征及其成藏意义[J].石油学报,2009,30(6):816-823.
[2]康玉柱,康志宏.塔里木盆地构造演化与油气[J].地球学报,1994,15(3/4):180-191.
[3]陆克政,漆家福,戴俊生.渤海湾新生代含油气盆地构造模式[M].北京:地质出版社,1997:1-50.
[4]Macgregor D S.Factors controlling the destruction or preservationof giant light oilfields[J].Petroleum Geoscience,1996,2:197-217.
[5]汪伟光,喻莲,宋成鹏,等.委内瑞拉马拉开波盆地构造演化对油气的控制[J].现代地质,2012,26(1):131-138.
[6]吴永平,付立新,杨池银,等.黄骅坳陷中生代构造演化对潜山油气成藏的影响[J].石油学报,2002,23(2):16-21.
[7]冯建伟,戴俊生,葛盛权.准噶尔盆地乌夏断裂带构造演化及油气聚集[J].中国石油大学学报:自然科学版,2008,32(3):23-29.
[8]Blanc J.Reservation,degradation and destruction of traped oil[M]//MagoonL B,Dow W G.The Petroleum System:fromSource to Trap.Tusler:AAPG,1994:73-89.
[9]何海清,王兆云,韩品龙.华北地区构造演化对渤海湾油气形成和分布的控制[J].地质学报,1998,72(4):313-321.
[10]邹华耀,向龙斌,梁宏斌,等.冀中坳陷潜山油气运聚动力学特征及其类型[J].地球科学:中国地质大学学报,2001,26(1):67-72.
[11]苏立萍,罗平,邹伟宏,等.冀中坳陷斜坡带奥陶系潜山油气成藏条件分析[J].大地构造与成矿学,2003,27(2):191-196.
[12]孙冬胜,刘池阳,杨明慧,等.渤海湾盆地冀中坳陷中区中新生代复合伸展构造[J].地质论评,2004,50(5):484-491.
[13]袁选俊,靳久强,孟庆仁,等.冀中坳陷杨村斜坡结构成因及油气成藏模式[J].石油学报,2004,25(4):19-22.
[14]于炳松,樊太亮.塔里木盆地寒武系—奥陶系泥质烃源岩发育的构造和沉积背景控制[J].现代地质,2008,22(4):534-539.
[15]崔军平,任战利.内蒙古海拉尔盆地乌尔逊凹陷热演化史[J].现代地质,2011,25(4):668-674.
[16]孙永河,漆家福,吕延防,等.渤中坳陷断裂构造特征及其对油气的控制[J].石油学报,2008,29(5):669-675.
[17]金涛,罗传容,吴亚军.岩溶作用对沙雅隆起奥陶系碳酸盐岩储集层的控制作用[J].沉积与特提斯地质,2001,21(1):27-32.
[18]牛玉静,康志宏,龙旭,等.塔河油田奥陶系岩溶油藏溶洞储集体成因及演化[J].现代地质,2011,25(4):650-659.
[19]林会喜.济阳坳陷桩西埕岛地区下古生界潜山储层岩溶作用[J].成都理工大学学报:自然科学版,2004,31(5):490-497.
[20]陈景山,李忠,王振宇,等.塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布[J].沉积学报,2007,25(6):858-868.
[21]杜学斌,解习农,任建业,等.济阳坳陷中生界古潜山油藏输导体系及成藏模式[J].地质科技情报,2005,24(2):22-26.
[22]孟卫工,陈振岩,李湃,等.潜山油气藏勘探理论与实践:以辽河坳陷为例[J].石油勘探与开发,2009,36(2):136-143.
[23]代寒松,赵锡奎,刘树根,等.塔里木盆地雅克拉断凸前中生界潜山构造与油气成藏[J].新疆石油地质,2009,30(1):17-20.
[24]付兆辉,高喜龙,陆友明,等.渤海湾盆地垦东凸起构造特征与油气聚集[J].现代地质,2008,22(4):619-627.
[25]于福生,阿木古冷,杨光达,等.准噶尔盆地车—莫古隆起的构造演化特征及其成因模拟[J].地球学报,2008,29(1):39-44.
[26]杨明慧.渤海湾盆地变换构造特征及其成藏意义[J].石油学报,2009,30(6):816-823.
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