新疆天山(独山子)-西昆仑(泉水沟)地学断面地震与重力联合反演地壳构造特征
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摘要
利用滑动平均的布格重力异常剖面结合地震资料和大地电磁资料 ,参考介质纵波速度与密度的经验转换关系 ,通过二维均匀介质模型人机交互式计算得到了新疆天山 (独山子 ) 西昆仑 (泉水沟 )地学断面走廊域中心剖面的地壳构造特征。所得的反演结果表明 ,准噶尔盆地与北天山地体、中天山地体为一整体 ;准噶尔盆地和天山构造带的中、下地壳之间存在低密度层 ,但塔里木盆地不存在低密度层 ;由于受到南北两侧板块挤压 ,造成塔里木盆地的地壳结构在横向上似一南陡北缓、中部隆起的不对称“拱形”弯曲 ;塔里木盆地南缘与西昆仑构造带间呈“V型盆山耦合关系” ,其下方恰好是莫霍面上隆区。
Based on the filetered Bouguer gravity anomaly, seismic data and telluric electromagnetic sounding data, the features of crustal structures of the corridor central profile in Tianshan(Dushanzi) West Kunlun(Quanshuigou) GGT are recognized by using modified empirical formula for the relationship between compressional velocity and density as well as the forward formula of uniform media for the two dimensional polygonal model. The inverse results suggest that North Tianshan, Central Tianshan and Junggar Basin are a monolithic body, and that a relatively low density layer exists between the middle and the lower crust in Jungar basin and Tianshan tectonic belt but does not exist in Tarim basin. As the Tarim basin is compressed by plates on both sides, i.e., Kazakstan Plate on the north and Indian Plate on the south, it looks like an asymmetrical arc, being wider in the North, steeper in the south and upwarped in the middle of the Tarim basin. The V shape coupling relationship between the basin and the range is located between the Tarim basin and the West Kunlun tectonic belt, just above the upwarped area of Moho.
Based on the filetered Bouguer gravity anomaly, seismic data and telluric electromagnetic sounding data, the features of crustal structures of the corridor central profile in Tianshan(Dushanzi) West Kunlun(Quanshuigou) GGT are recognized by using modified empirical formula for the relationship between compressional velocity and density as well as the forward formula of uniform media for the two dimensional polygonal model. The inverse results suggest that North Tianshan, Central Tianshan and Junggar Basin are a monolithic body, and that a relatively low density layer exists between the middle and the lower crust in Jungar basin and Tianshan tectonic belt but does not exist in Tarim basin. As the Tarim basin is compressed by plates on both sides, i.e., Kazakstan Plate on the north and Indian Plate on the south, it looks like an asymmetrical arc, being wider in the North, steeper in the south and upwarped in the middle of the Tarim basin. The V shape coupling relationship between the basin and the range is located between the Tarim basin and the West Kunlun tectonic belt, just above the upwarped area of Moho.
引文
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高锐,黄东定,卢德源等.2000.横过西昆仑造山带与塔里木盆地结合带的深地震反射剖面.科学通报,45(17):1874～1879.
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李秋生,卢德源,高锐等.2000.横跨西昆仑塔里木接触带的爆炸地震探测.中国科学(D),30(增刊):16～21.
卢德源,李秋生,高锐等.2000.横跨天山的人工爆炸地震剖面.科学通报,45(9):982～987.
秦国卿,陈九辉,刘大建等.1994.昆仑山脉和喀拉昆仑山脉的地壳上地幔电性结构.地球物理学报,37(2):193～199.
魏素花,薛光琦,钱辉等.2000.新疆库车克拉玛依地震层析成像.地球物理学进展,15(4):46～54.
新疆维吾尔自治区地质矿产局.1993.新疆维吾尔自治区区域地质志.北京:地质出版社.胥颐,刘富田,刘建华等.2000.中国大陆西北造山带及其毗邻盆地的地震层析成像.中国科学(D),30(2):113～122.
胥颐,刘富田,刘建华等.2001.中国西北大陆碰撞带的深部特征及其动力学意义.地球物理学报,44(1):40～47.
尹安.2001.喜马拉雅青藏高原造山带地质演化.地球学报,22(3):193～230.
DingDaogui,TangLiangjieetal..1996.Formationandtectonicevolu tionoftheTarimbasin.Nanjing:HehaiUniversityPress(inChi nese).
GuanYe,GaoHong,GaoRuietal..2001.TheexpermentsofboadbandseisrnicstudyalongTarimtoKunlun.ActaGeoscientiasinica,22(6):559～562(inChinese).
FanG ,NiJF ,WallaceTC .1986.ActivetectonicsofthePamirsandKarakorum.JGeophysRes,(99):7131～7160.
FengRui,YanHuifen,ZhangRuoshui.1986.Afastinversemethodofthree dimensionalpotentialfieldanditsprogramdesign.J.Geolo gy,(4):390～402(inChinese).
GaoJun,LiMaosong,XiaoXuchangetal..1998.PaleozonictectonicevolutionoftheTianshanOrogen,NorthwesternChina.Tectono physics,287(287):213～231.
GaoRui,HuangDongding,LuDeyuanetal..2000.Adeepseismicre flectionprofileacrosstheconjunctionzonebetweenWestKunlunMountainsandTarimbasin.ChineseScienceBulletin,45(17):1874～1879(inChinese).
LiQiusheng,LuDeyuan,GaoRuietal..2000.AnexplosiveseismicsoundingprofileacrossthetransitionzonebetweenWestKunlunMts.andTarimbasin.ScienceinChina(SeriesD),30(Sup.):16～21(inChinese).
LuDeyuan,LiQiusheng,GaoRuietal..2000.Adeepseismicsoun dingprofileacrosstheTianshanMountains.ChineseScienceBul letin(D),45(9):982～987(inChinese).
QinGuoqing,ChenJiuhui,LiuDajianetal..1994.TheCharacteristicsoftheelectricalstructureofthecrustanduppermantleinthere gionoftheKunlunandtheKarakorumMountains.ChineseJ.Geo phys,37(2):193～199(inChinese).
WatsonMP ,HaywardAB ,ParkinsonDNetal..1987.Platetectonichistory,basindevelopmentandpetroleumsourcerockdepositiononshoreChina.Mar.Pet.Geol.,(4):205～225.
WeiSuhua,XueGuangqi,QianHuietal..2000.XinjiangKucheKela mayiseimictomography.ProgressinGeophysics,15(4):46～54(inChinese).
XinjiangBureauofGeologyandMineralResouces.1993.Regionalgeo logyofXinjiangUygurAutonomousRegion.Bejing:GeologicalPublishingHouse(inChinese).
XuYi,LiuFutian,LiuJianhuaetal..2000.Seismictomographybe neathnorthwesternorogenicbeltsandadjacentbasinsinChinesecontinent.ScienceinChina,30(2):113～122(inChinese).
XuYi,LiuFutian,LiuJianhuaetal..2001.Deepfeaturesofcontinen talcollisionbeltsinnorthwesternChinaandtheirdynamicimplica tions.ChineseJ.Geophysics,44(1):40～47(inChinese).
YinA ,SNie,PCraigetal..1998.LateCenozoictectonicevolutionofthesouthernChineseTianshan.Tectonics,17(1):1～27.
YinA .2001.GeologicalevolutionoforogeninHimalayaTibetPlateau.ActaGeoscientaSinica,22(3):193～230(inChinese).
YuanX ,ZhoY ,ZhangC .1994.EvidencesforthewestChinacratonsanditsevolution.Proc.29thint.Geol.Congr.PartB ,39～51.
ZhangZM ,LiouoJG ,ColemanRG .1984.AnoutlineoftheplatetectonicsofChina.Geol.Soc.Am.Bull.,95:295～312.
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