早白垩世合肥盆地性质及含油气性分析
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摘要
根据地震、电法、盆地模拟等新资料并结合区域地质资料的综合分析,对早白垩世合肥盆地的复杂构造及盆地性质、演化进行了深入讨论,认为合肥盆地在早白垩世时属于一个处于由压性应力场向张性应力场转换过程中形成的复杂复合盆地,即早白垩世早中期属主要受控于其南侧大别造山带的滑覆冲断类前陆盆地、早白垩世中晚期属主要受控于其东侧郯庐断裂活动的走滑拉分盆地。进而探讨了其拉分盆地内潜在的下白垩统油气系统及其勘探前景。从盆地研究的角度来进一步认识郯庐断裂的活动及对合肥盆地的油气勘探均具有借鉴及指导意义。
New data including seismic data, MT data and the basin simulation data as well as the regional geologic data indicate that Hefei Basin in Early Cretaceous was a composite basin. This basin was formed after the similar forland basin in the Jurassic and before the fault basin in the Late Cretaceous Early Tertiary, so it was complicated in the transitional stress field from the compression to the strike slip. It can be divided into two parts, one is the sliding thrust similar foreland basin which was controlled by the Dabie Orogenic Belt in the early middle period of Early Cretaceous, the other is the pull apart basin which was mainly controlled by the Tan Lu Fault Zone in the middle late period of Early Cretaceous. In the pull apart basin, there exists a potential Lower Cretaceous petroleum system. For lack of certain traps, so there is a risk for exploration. It is instructive to realize the movement of the Tan Lu Fault System and its influence on the Hefei Basin from the view point of basin research.
New data including seismic data, MT data and the basin simulation data as well as the regional geologic data indicate that Hefei Basin in Early Cretaceous was a composite basin. This basin was formed after the similar forland basin in the Jurassic and before the fault basin in the Late Cretaceous Early Tertiary, so it was complicated in the transitional stress field from the compression to the strike slip. It can be divided into two parts, one is the sliding thrust similar foreland basin which was controlled by the Dabie Orogenic Belt in the early middle period of Early Cretaceous, the other is the pull apart basin which was mainly controlled by the Tan Lu Fault Zone in the middle late period of Early Cretaceous. In the pull apart basin, there exists a potential Lower Cretaceous petroleum system. For lack of certain traps, so there is a risk for exploration. It is instructive to realize the movement of the Tan Lu Fault System and its influence on the Hefei Basin from the view point of basin research.
引文
安徽省地质矿产局.1987.安徽省区域地质志.北京:地质出版社.
邓乃恭,任希飞.1996.造山与成盆作用形成于统一的动力学机制.地质论评,42(4):300-303.
高大旗.1992.安徽磨子潭—晓天地区中生代火山岩的时空分布及火山喷发旋回.安徽地质,2(3):20-27.
介霖.1992.中国石油地质志(卷八)———苏浙皖闽油气区.北京:石油工业出版社,398-410.
李玉发,姜立富.1997.安徽省岩石地层———全国地层多重划分对比研究(34).武汉:中国地质大学出版社.
宋明水,江来利,李学田,储东如,杜森官.2002.大别山造山带对合肥盆地的构造控制.石油实验地质,24(3):209-215.
汤加富,孙先如,荆延仁,侯明金,高天山,周存亭.1995.安徽大别山—张八岭地区新的构造格局与非板块碰撞造山过程.安徽地质,5(3):1-12.
王果胜,段翔,谭应佳.1997.豫皖交界中新生代地层特征及盆地演化.现代地质,11(2):229-235.
王清晨,从柏林,马力.1997.大别山造山带与合肥盆地的构造耦合.科学通报,42(6):575-580.
吴跃东,侯明金,刘家云.1999.合肥盆地东北缘白垩纪地层特征及沉积环境分析.安徽地质,9(2):102-107.
薛爱民,金维浚,袁学诚.1999.大别山北缘合肥盆地中、新生代构造演化.高校地质学报,5(2):157-163.
杨坤光,马昌前,许长海,杨巍然.1999.北淮阳构造带与大别造山带的差异性隆升.中国科学(D辑),29(2):97-103.
张永军,黄钟瑾.1998.张八岭推覆体特征及其成因机制.高校地质学报,4(4):444-451.
赵宗举,李大成,朱琰,周进高,冯加良.2001.合肥盆地构造演化及油气系统.石油勘探与开发,28(4):8-13.
赵宗举,杨树锋,陈汉林,竺国强,楼章华.2000.合肥盆地基底构造属性.地质科学,35(3):288-296.
周进高,赵宗举,邓红婴.1999.合肥盆地构造演化及其含油气性分析.地质学报,73(1):15-23.朱光,牛漫兰,刘国生,王道轩,宋传中.2002.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-333.
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学(D辑),31(3):250-256.
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452-456.AnhuiBureauofGeologyandMineralResources.1987.BrieftextinEnglishofregionalgeologyofAnhuiProvince.Beijing:GeologicalPublishingHouse(inChinese).
DengNaigongandRenXifei.1996.Formationofmountainrangesandbasinsinauniteddynamicmechanism.GeologicalReview,42(4):300-303(inChinesewithEnglishabstract).
GaoDaqi.1992.ThetemporalandspatialdistributionoftheMesozonicvolcanicsandthedivisionofvolcaniceruptioncyclesintheMozitan-XiaotianArea,Anhui.GeologyofAnhui,2(3):20-27(inChinesewithEnglishabstract).JieLin.1992.PetroleumGeologyofChina(Vol.8).
Beijing:PetroindustryPublishingHouse,398-410(inChinese).LiYufaandJiangLifu.1997.PetrostratigraphyinAnhuiProvince.Wuhan:PressofChinaUniversityofGeoscience(inChinese).
SongMinshui,JiangLaili,LiXuetian,ChuDongruandDuSenguan.2002.TectoniccontroloftheDabieshanoroge-nicBeltovertheHefeiBasin.PetroleumGeology&Experiment,24(3):209-215(inChinesewithEnglishabstract).
TangJiafu,SunXianru,JingYanren,HouMingjin,GaoTianshanandZhouCunting.1995.NewtectonicframeworkoftheDabie-Zhangbalingareaandnon-plate-collisionorogene-sis.GeologyofAnhui,5(3):1-12(inChinesewithEnglishabstract).
WangGuosheng,DuanXiangandTanYingjia.1997.Stratigra-phicfeaturesoftheMeso-CenozoicinAnhui-Henanborderareaandbasin’sevolution.Geoscience,11(2):229-235(inChinesewithEnglishabstract).
WangQingchen,CongBolinandMaLi.1997.TectoniccouplingbetweenDabieorogenicbeltandHefeiBasin.ChineseSciBull,42(6):575-580(inChinese).
WuYuedong,HouMingjinandLiuJiayun.1999.ThefeaturesandsedimentaryenvironmentalanalysisoftheCretaceousstrataonthenortheastmarginofHefeiBasin.GeologyofAnhui.9(2):102-107(inChinesewithEnglishabstract).
XueAimin,JinWeijunandYuanXuecheng.1999.TectonicevolutionofHefeiBasin,northernDabieMountainsintheMesozoicandtheCenozoic.GeologicalJournalofChinaUniversities,5(2):157-163(inChinesewithEnglishabstract).
YangKunguang,MaChangqian,XuChanghaiandYangWeiran.1999.DifferentialupliftbetweenBeihuaiyangtectoniczoneandDabieOrogenicBelt.ScienceinChina(SeriesD),29(2):97-103(inChinese).
ZhangYongjunandHuangZhongjin.1998.Geometryandme-chanicsofZhangbalingnappleineastofTan-LuFaultZone,EasternChina.GeologicalJournalofChinaUniver-sities,4(4):444-451(inChinesewithEnglishabstract).
ZhaoZongju,LiDacheng,ZhuYan,ZhouJingaoandFengJia-liang.2001.ThestructureevolutionandthepetroleumsysteminHefeiBasin.PetroleumExplorationandDevelop-ment,28(4):8-13(inChinesewithEnglisha
邓乃恭,任希飞.1996.造山与成盆作用形成于统一的动力学机制.地质论评,42(4):300-303.
高大旗.1992.安徽磨子潭—晓天地区中生代火山岩的时空分布及火山喷发旋回.安徽地质,2(3):20-27.
介霖.1992.中国石油地质志(卷八)———苏浙皖闽油气区.北京:石油工业出版社,398-410.
李玉发,姜立富.1997.安徽省岩石地层———全国地层多重划分对比研究(34).武汉:中国地质大学出版社.
宋明水,江来利,李学田,储东如,杜森官.2002.大别山造山带对合肥盆地的构造控制.石油实验地质,24(3):209-215.
汤加富,孙先如,荆延仁,侯明金,高天山,周存亭.1995.安徽大别山—张八岭地区新的构造格局与非板块碰撞造山过程.安徽地质,5(3):1-12.
王果胜,段翔,谭应佳.1997.豫皖交界中新生代地层特征及盆地演化.现代地质,11(2):229-235.
王清晨,从柏林,马力.1997.大别山造山带与合肥盆地的构造耦合.科学通报,42(6):575-580.
吴跃东,侯明金,刘家云.1999.合肥盆地东北缘白垩纪地层特征及沉积环境分析.安徽地质,9(2):102-107.
薛爱民,金维浚,袁学诚.1999.大别山北缘合肥盆地中、新生代构造演化.高校地质学报,5(2):157-163.
杨坤光,马昌前,许长海,杨巍然.1999.北淮阳构造带与大别造山带的差异性隆升.中国科学(D辑),29(2):97-103.
张永军,黄钟瑾.1998.张八岭推覆体特征及其成因机制.高校地质学报,4(4):444-451.
赵宗举,李大成,朱琰,周进高,冯加良.2001.合肥盆地构造演化及油气系统.石油勘探与开发,28(4):8-13.
赵宗举,杨树锋,陈汉林,竺国强,楼章华.2000.合肥盆地基底构造属性.地质科学,35(3):288-296.
周进高,赵宗举,邓红婴.1999.合肥盆地构造演化及其含油气性分析.地质学报,73(1):15-23.朱光,牛漫兰,刘国生,王道轩,宋传中.2002.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-333.
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学(D辑),31(3):250-256.
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452-456.AnhuiBureauofGeologyandMineralResources.1987.BrieftextinEnglishofregionalgeologyofAnhuiProvince.Beijing:GeologicalPublishingHouse(inChinese).
DengNaigongandRenXifei.1996.Formationofmountainrangesandbasinsinauniteddynamicmechanism.GeologicalReview,42(4):300-303(inChinesewithEnglishabstract).
GaoDaqi.1992.ThetemporalandspatialdistributionoftheMesozonicvolcanicsandthedivisionofvolcaniceruptioncyclesintheMozitan-XiaotianArea,Anhui.GeologyofAnhui,2(3):20-27(inChinesewithEnglishabstract).JieLin.1992.PetroleumGeologyofChina(Vol.8).
Beijing:PetroindustryPublishingHouse,398-410(inChinese).LiYufaandJiangLifu.1997.PetrostratigraphyinAnhuiProvince.Wuhan:PressofChinaUniversityofGeoscience(inChinese).
SongMinshui,JiangLaili,LiXuetian,ChuDongruandDuSenguan.2002.TectoniccontroloftheDabieshanoroge-nicBeltovertheHefeiBasin.PetroleumGeology&Experiment,24(3):209-215(inChinesewithEnglishabstract).
TangJiafu,SunXianru,JingYanren,HouMingjin,GaoTianshanandZhouCunting.1995.NewtectonicframeworkoftheDabie-Zhangbalingareaandnon-plate-collisionorogene-sis.GeologyofAnhui,5(3):1-12(inChinesewithEnglishabstract).
WangGuosheng,DuanXiangandTanYingjia.1997.Stratigra-phicfeaturesoftheMeso-CenozoicinAnhui-Henanborderareaandbasin’sevolution.Geoscience,11(2):229-235(inChinesewithEnglishabstract).
WangQingchen,CongBolinandMaLi.1997.TectoniccouplingbetweenDabieorogenicbeltandHefeiBasin.ChineseSciBull,42(6):575-580(inChinese).
WuYuedong,HouMingjinandLiuJiayun.1999.ThefeaturesandsedimentaryenvironmentalanalysisoftheCretaceousstrataonthenortheastmarginofHefeiBasin.GeologyofAnhui.9(2):102-107(inChinesewithEnglishabstract).
XueAimin,JinWeijunandYuanXuecheng.1999.TectonicevolutionofHefeiBasin,northernDabieMountainsintheMesozoicandtheCenozoic.GeologicalJournalofChinaUniversities,5(2):157-163(inChinesewithEnglishabstract).
YangKunguang,MaChangqian,XuChanghaiandYangWeiran.1999.DifferentialupliftbetweenBeihuaiyangtectoniczoneandDabieOrogenicBelt.ScienceinChina(SeriesD),29(2):97-103(inChinese).
ZhangYongjunandHuangZhongjin.1998.Geometryandme-chanicsofZhangbalingnappleineastofTan-LuFaultZone,EasternChina.GeologicalJournalofChinaUniver-sities,4(4):444-451(inChinesewithEnglishabstract).
ZhaoZongju,LiDacheng,ZhuYan,ZhouJingaoandFengJia-liang.2001.ThestructureevolutionandthepetroleumsysteminHefeiBasin.PetroleumExplorationandDevelop-ment,28(4):8-13(inChinesewithEnglisha
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