中国陆相湖盆震积岩研究综述
摘要
本文主要回顾了震积岩的研究现状,特别是我国对其研究起步较早,但主要集中于前中生代海相地层的研究,九十年代以来越来越多的学者注意到在陆相中生代以来的地层中也发育有震积岩,其研究意义不亚于海相震积岩,特别是在油气储存方面具有不可估量的研究价值,因而掀起研究热潮,目前对中国东部新生代断陷盆地古近纪碎屑岩的研究比较详细。研究发现地震作为一种自然灾变事件,六级以上的强震作用才能在地层中形成震积岩并保存下来,但根据影响性质差异其识别标志可划分为两种,即直接标志和与地震有关的辅助标志,各个标志中又包括多种类型,并依据各类型组合特征划分多种震积岩垂向序列。陆相震积岩的研究意义主要表现在震积岩作为重要地质事件沉积的代表,有助于理解和认识控盆构造作用及其演化特征,是一种潜在的储集类型及等时地层界面,并结合层序地层学等其他学科的理论,可形成新的学科。
引文
[1]G.R.SHI,Y.S.DU AND Y.M.GONG.Soft-sediment deforma-tion structures interpreted as seismite from the Middle Permian of thesouthern Sydney Basin,southeastern Australia[J].Australian Journal ofEarth Sciences,2007,54:861-874.
[2]杜元生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.
[3]Seilacher A.Fault-grade bed Interpreted as seismites[J].Sedmen-tology,1969,13(1-2):155-159.
[4]SpalletaC,VaiGB.UpperDevonianintraclastparabrecciasinte-rpret-ed as seismite[s J].Marine Geology,1984,55(1-2):133-144.
[5]Seilacher A.Sedimentary structures tentatively attributed to seis-micevent[s J].Marine Geology,1984,55(1-2):1-12.
[6]Gerhard H.Bachmann,Mahmoud A.M.Aref.A seismite in Tri-assic gypsum deposits(Grabfeld Formation,Ladinian),southwestern Ger-many[J].Sedimentary Geology,2005,180:75-89.
[7]Jones,A.P.and Omoto,K.Towards establishing criteria for identi-fying trigger mechanisms for soft-sediment deformation:a case study ofLate Pleistocene lacustrine sand clays,Onikobe and Nakaymadaira basins,northeastern Japan.Sedimentology,2000,47:1211-1226.
[8]Rossetti,D.F.,Goes,A.M.Deciphering the sedimentological im-print of paleoseismic events:an example from the Aptian Codo Formation,northern Brazi[l J].Sediment.Geol,2000,135:137-156.
[9]M.Moretti,P.Alfarob,O.Caselles c,et,al.Modelling seismiteswith a digital shaking table[J].Tectonophysics,1999,304:369-383.
[10]宋天锐.北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震-海啸序列.科学通报,1988,38(8):609-611.
[11]Du YuansHeng,ZHANG Chuanheng,HAN Xin,et al.Earth-quake event deposits in Mesoproterozoic Kunyang Group in central Yun-nan Province and its geological implications[J].SCIENCEINCHINA(Se-riesD),2001,7:600-608.
[12]乔秀夫,宋天锐,高林志等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):1-34.
[13]乔秀夫,宋天锐,高林志等.中国震积岩的研究与展望[J].地质论评,1996,42(4):317-320.
[14]Rajat Mazumder,A.J.(Tom)vanLoon,MakotoArima.So ft-sediment deformation structures in the Earth’s oldest seismite[J].Sedi-mentaryGeology,2006.20:19-26.
[15]孙晓猛,梁定益,聂泽同.大陆边缘震积岩序列——以金沙江中段震积岩为例[J].现代地质,1995,9(3):1-27.
[16]贾志海,洪天求,郑文武等.皖北新元古代望山组震积岩的基本特征及其形成环境分析[J].地层学杂志,2007,27(2):146-151.
[17]吴贤涛,尹国勋.四川峨眉晚侏罗世湖泊沉积中震积岩的发现及其意义[J].沉积学报,1992,10(3):19-24.
[18]梁定益,聂泽同,万晓摭.试论震积岩及震积不整合——以川西、滇西地区为例[J].现代地质,1991,5(2):138-147.
[19]梁定益,聂泽同,宋志敏.再论震积岩及震积不整合——以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[20]乔秀夫,高林志,彭阳等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑),2001,31(11):911-918.
[21]郭建华,王方平,刘贵等.湘西大庸上震旦统灯影组震裂角砾岩[J].石油实验地质,1999,21(3):219-224.
[22]尹国勋,汤友谊.地史时期地震事件的岩石学证据——以四川峨嵋晚侏罗世湖泊沉积中的震积岩为例[J].地震地质,1993,15(1):61-65.
[23]张琴,朱筱敏,张建军等.酒西盆地青南凹陷柳沟庄—窟窿山地区下白垩统震积岩的发现及意义[J].地质学报,2003,77(2):158-162.
[24]陈世悦,袁文芳,鄢继华.济阳坳陷早第三纪震积岩的发现及其意义[J].地质科学,2003,38(3):413-424.
[25]杨剑萍,王辉,陈世悦等.济阳坳陷古近系震积岩特征[J].沉积学报,2004,22(2):281-286.
[26]袁静.山东惠民凹陷古近纪震积岩特征及其地质意义[J].沉积学报,2004,22(1):41-46.
[27]杨剑萍,王亚丽,查明等.山东惠民凹陷古近系湖泊地震涌浪记录的新发现[J].地质学报,2006,80(11):1715-1722.
[28]夏青松,田景春.鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义[J].沉积学报,2007,25(2):246-252.
[29]袁静.中国震积作用和震积岩研究进展[J].石油大学学报(自然科学版),2005,29(1):144-149.
[30]王化爱,钟建华,陈鑫等.飞蒙古塔木察格坳陷白垩系震积岩特征及其地质意义[J].地质学报,2008,82(8):1088-1094.
[31]王昌勇,郑荣才,高振中.准噶尔盆地下侏罗统八道湾组震积岩的发现及其研究意义[J].地质论评,2008,54(6):821-826.
[32]吕洪波,章雨旭,夏邦栋等.南盘江盆地中三叠统复理石中的同沉积挤压构造——类新的沉积构造的归类、命名和构造意义探讨[J].地质论评,2003,49(5):449-456.
[33]吕洪波,章雨旭,肖国望等.内蒙古白云鄂博南东黑脑包腮林忽洞群下部发现地震滑塌岩块[J].地质论评,2006,52(2):163-169.
[34]黄宏伟,杜远生,黄志强等.广西丹池盆地晚古生代震积岩及其构造意义[J].地质论评,2007,53(5):592-511.
[35]Moretti M.Soft-sediment deformation structures interpreted asseismites in middle-late Pleistocene aeolian foreland,southern Italy[J].Sedimentary Geology,2000,135(1-4):167-179.
[36]Rodriguez PMA,Calvo J P,De Vicente J et,al.Soft sedimentdeformation structures interpreted as seismites in lacustrine sediments of thePrebetic Zone,SE Spain,and their potential use as indicators of earthquakemagnitudes duringthe Late Miocene[J].Sedimentary Geology,2000,135(1-4):117-135.
[37]Rodriguez PMA,Calvo J P and Perez-Lopez R.Similarities be-tween recent seismic activity and paleoseismites during the Late Miocene inthe external Betlc Chain(Spain):relationship by‘b’value and the fractal di-mension[J].Jour.Struc.Geol,2002.,4:117-135.
[38]Obermeier,S.F.Use of liquefaction-induced features for paleo-seismic analysis—an overview of how liquefaction features can be distin-guished from other features and how their distribution and properties ofsource sediment can be used to infer the location and strength of Holocenepaleo-earthquake[s J].Eng.Geol.1996,44,1-76.
[39]Takashimizu Y and Masuda F.Depositional facies and sedimen-tary successions of earthquake2induced tsunami deposits in Up-per Pleisto-cene incised valley fills,central Japan[J].Sedimentary Geology,2000,135(1-4):231-239.
[40]贾松,彭军,刘建锋.国内震积岩研究现状[J].地质灾害与环境保护,2006,17(1):39-44.
[41]宫丽清,杨剑萍.济阳坳陷古近系沙河街组震积岩特征及其储集性能[J].新疆石油地质,2007,28(1):44-47.
[42]杨仕维,李建明.震积岩特征综述及地质意义[J].岩性油气藏,2008,20(1):89-94.
[43]赵卫卫,查明,杨剑萍.中国震积岩研究综述[J].地层学杂志,2006,30(2):171-176.
[44]曹国强,陈世悦,鄢继华等.济阳坳陷早第三纪地震事件沉积序列[J].地质找矿论丛,2004,19(4):252-256.
[45]付文利,王艳琴,杨光等.东营凹陷沙三段、沙四段震积岩研究[J].油气地质与采收率,2004,11(2):6-8.
[46]HelenE.Jewell,FrankR.Ettensohn.AnancientseismiteresponsetoTaconianfar-fieldforces:TheCaneRunBed,UpperOrdovician(Trenton)LexingtonLimestone,centralKentucky(USA)[J].SedimentaryGeology,2004,37:487-511.
[47]LuizAlbertoFernandes,AliceBonattodeCastro,,GiorgioBasilici.SeismitesincontinentalsandseadepositsoftheLateCretaceousCaiuaDesert,Bauru-Basin,Braz[i J].SedimentaryGeology,2007,199:51-64.
[48]李元昊,刘池洋,王秀娟.鄂尔多斯盆地三叠系延长组震积岩特征研究[J].沉积学报,2008,26(5):772-779.
[2]杜元生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,15(4):389-394.
[3]Seilacher A.Fault-grade bed Interpreted as seismites[J].Sedmen-tology,1969,13(1-2):155-159.
[4]SpalletaC,VaiGB.UpperDevonianintraclastparabrecciasinte-rpret-ed as seismite[s J].Marine Geology,1984,55(1-2):133-144.
[5]Seilacher A.Sedimentary structures tentatively attributed to seis-micevent[s J].Marine Geology,1984,55(1-2):1-12.
[6]Gerhard H.Bachmann,Mahmoud A.M.Aref.A seismite in Tri-assic gypsum deposits(Grabfeld Formation,Ladinian),southwestern Ger-many[J].Sedimentary Geology,2005,180:75-89.
[7]Jones,A.P.and Omoto,K.Towards establishing criteria for identi-fying trigger mechanisms for soft-sediment deformation:a case study ofLate Pleistocene lacustrine sand clays,Onikobe and Nakaymadaira basins,northeastern Japan.Sedimentology,2000,47:1211-1226.
[8]Rossetti,D.F.,Goes,A.M.Deciphering the sedimentological im-print of paleoseismic events:an example from the Aptian Codo Formation,northern Brazi[l J].Sediment.Geol,2000,135:137-156.
[9]M.Moretti,P.Alfarob,O.Caselles c,et,al.Modelling seismiteswith a digital shaking table[J].Tectonophysics,1999,304:369-383.
[10]宋天锐.北京十三陵前寒武纪碳酸盐岩地层中的一套可能的地震-海啸序列.科学通报,1988,38(8):609-611.
[11]Du YuansHeng,ZHANG Chuanheng,HAN Xin,et al.Earth-quake event deposits in Mesoproterozoic Kunyang Group in central Yun-nan Province and its geological implications[J].SCIENCEINCHINA(Se-riesD),2001,7:600-608.
[12]乔秀夫,宋天锐,高林志等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):1-34.
[13]乔秀夫,宋天锐,高林志等.中国震积岩的研究与展望[J].地质论评,1996,42(4):317-320.
[14]Rajat Mazumder,A.J.(Tom)vanLoon,MakotoArima.So ft-sediment deformation structures in the Earth’s oldest seismite[J].Sedi-mentaryGeology,2006.20:19-26.
[15]孙晓猛,梁定益,聂泽同.大陆边缘震积岩序列——以金沙江中段震积岩为例[J].现代地质,1995,9(3):1-27.
[16]贾志海,洪天求,郑文武等.皖北新元古代望山组震积岩的基本特征及其形成环境分析[J].地层学杂志,2007,27(2):146-151.
[17]吴贤涛,尹国勋.四川峨眉晚侏罗世湖泊沉积中震积岩的发现及其意义[J].沉积学报,1992,10(3):19-24.
[18]梁定益,聂泽同,万晓摭.试论震积岩及震积不整合——以川西、滇西地区为例[J].现代地质,1991,5(2):138-147.
[19]梁定益,聂泽同,宋志敏.再论震积岩及震积不整合——以川西、滇西地区为例[J].地球科学,1994,19(6):845-850.
[20]乔秀夫,高林志,彭阳等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑),2001,31(11):911-918.
[21]郭建华,王方平,刘贵等.湘西大庸上震旦统灯影组震裂角砾岩[J].石油实验地质,1999,21(3):219-224.
[22]尹国勋,汤友谊.地史时期地震事件的岩石学证据——以四川峨嵋晚侏罗世湖泊沉积中的震积岩为例[J].地震地质,1993,15(1):61-65.
[23]张琴,朱筱敏,张建军等.酒西盆地青南凹陷柳沟庄—窟窿山地区下白垩统震积岩的发现及意义[J].地质学报,2003,77(2):158-162.
[24]陈世悦,袁文芳,鄢继华.济阳坳陷早第三纪震积岩的发现及其意义[J].地质科学,2003,38(3):413-424.
[25]杨剑萍,王辉,陈世悦等.济阳坳陷古近系震积岩特征[J].沉积学报,2004,22(2):281-286.
[26]袁静.山东惠民凹陷古近纪震积岩特征及其地质意义[J].沉积学报,2004,22(1):41-46.
[27]杨剑萍,王亚丽,查明等.山东惠民凹陷古近系湖泊地震涌浪记录的新发现[J].地质学报,2006,80(11):1715-1722.
[28]夏青松,田景春.鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义[J].沉积学报,2007,25(2):246-252.
[29]袁静.中国震积作用和震积岩研究进展[J].石油大学学报(自然科学版),2005,29(1):144-149.
[30]王化爱,钟建华,陈鑫等.飞蒙古塔木察格坳陷白垩系震积岩特征及其地质意义[J].地质学报,2008,82(8):1088-1094.
[31]王昌勇,郑荣才,高振中.准噶尔盆地下侏罗统八道湾组震积岩的发现及其研究意义[J].地质论评,2008,54(6):821-826.
[32]吕洪波,章雨旭,夏邦栋等.南盘江盆地中三叠统复理石中的同沉积挤压构造——类新的沉积构造的归类、命名和构造意义探讨[J].地质论评,2003,49(5):449-456.
[33]吕洪波,章雨旭,肖国望等.内蒙古白云鄂博南东黑脑包腮林忽洞群下部发现地震滑塌岩块[J].地质论评,2006,52(2):163-169.
[34]黄宏伟,杜远生,黄志强等.广西丹池盆地晚古生代震积岩及其构造意义[J].地质论评,2007,53(5):592-511.
[35]Moretti M.Soft-sediment deformation structures interpreted asseismites in middle-late Pleistocene aeolian foreland,southern Italy[J].Sedimentary Geology,2000,135(1-4):167-179.
[36]Rodriguez PMA,Calvo J P,De Vicente J et,al.Soft sedimentdeformation structures interpreted as seismites in lacustrine sediments of thePrebetic Zone,SE Spain,and their potential use as indicators of earthquakemagnitudes duringthe Late Miocene[J].Sedimentary Geology,2000,135(1-4):117-135.
[37]Rodriguez PMA,Calvo J P and Perez-Lopez R.Similarities be-tween recent seismic activity and paleoseismites during the Late Miocene inthe external Betlc Chain(Spain):relationship by‘b’value and the fractal di-mension[J].Jour.Struc.Geol,2002.,4:117-135.
[38]Obermeier,S.F.Use of liquefaction-induced features for paleo-seismic analysis—an overview of how liquefaction features can be distin-guished from other features and how their distribution and properties ofsource sediment can be used to infer the location and strength of Holocenepaleo-earthquake[s J].Eng.Geol.1996,44,1-76.
[39]Takashimizu Y and Masuda F.Depositional facies and sedimen-tary successions of earthquake2induced tsunami deposits in Up-per Pleisto-cene incised valley fills,central Japan[J].Sedimentary Geology,2000,135(1-4):231-239.
[40]贾松,彭军,刘建锋.国内震积岩研究现状[J].地质灾害与环境保护,2006,17(1):39-44.
[41]宫丽清,杨剑萍.济阳坳陷古近系沙河街组震积岩特征及其储集性能[J].新疆石油地质,2007,28(1):44-47.
[42]杨仕维,李建明.震积岩特征综述及地质意义[J].岩性油气藏,2008,20(1):89-94.
[43]赵卫卫,查明,杨剑萍.中国震积岩研究综述[J].地层学杂志,2006,30(2):171-176.
[44]曹国强,陈世悦,鄢继华等.济阳坳陷早第三纪地震事件沉积序列[J].地质找矿论丛,2004,19(4):252-256.
[45]付文利,王艳琴,杨光等.东营凹陷沙三段、沙四段震积岩研究[J].油气地质与采收率,2004,11(2):6-8.
[46]HelenE.Jewell,FrankR.Ettensohn.AnancientseismiteresponsetoTaconianfar-fieldforces:TheCaneRunBed,UpperOrdovician(Trenton)LexingtonLimestone,centralKentucky(USA)[J].SedimentaryGeology,2004,37:487-511.
[47]LuizAlbertoFernandes,AliceBonattodeCastro,,GiorgioBasilici.SeismitesincontinentalsandseadepositsoftheLateCretaceousCaiuaDesert,Bauru-Basin,Braz[i J].SedimentaryGeology,2007,199:51-64.
[48]李元昊,刘池洋,王秀娟.鄂尔多斯盆地三叠系延长组震积岩特征研究[J].沉积学报,2008,26(5):772-779.
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