简介：<正>ONINTEGRATIVEGEOTECTONICSChenGuoda(ChangshaInstituteofGeotectonics,AcademiaSinica,410003,Hunan,China)XiangJixi(TheChineseAcademyofGeologicalSciences,Beijing,China)integrativegeotectonics,crustobodygeotectonics,multi-originedandpolygeneticcompoundresultantforcesystem,tectosphere,gradualchange,mutation,catastrophismBasedonhistoristic-causationistgeotectonicsproposedbyChenGuodain1992,theauthorsattempttofurtherextenditscontentsandranges,establishintegrativegeo-tectonicswithwiderangesandhighersynthesis.Integrativegeotectonicsisdefinedasadisci-plinetostudyverysyntheticallythewholehistoryandcausationisticrelationsofformationandevolutionoftheglobaltectonics(includingthecrustalanddeepteetosphericstructures)withthecomprehensiveanalysismethod.Itisalsocalledas"crustobodygeotectonics"foritsmaingeotectonicelementiscrustobody.Itscharacteristicsare:(1)regardingtheinternalandexter-naldynamic

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简介：OIntroductionBypresent,soliddatabasehasbeengatheredonregionalmetallogenicstudiesonplate-tectonicbasis.Asformid-scaleandmoreoverlarge-scaleworks,theyarelessnumerous;methodologyandtypicalmodellingareatinitialstage,thoughfundamentalandappliedval-uesofthesestudiesarequiteevident.Theauthorshavetriedtodom

简介：AfterhavingreadCrustobodGeotectonicsofAsianContinentandAdjacentSeaswrittenbyProf.ChenGuodaetal-,Iamabsorbedinitsstrikingviewpoints,clearclue,abundantproofs,profoundandlastingconsiderationandrichcontents.Theyarechieflyshowninthefollowing:l.Fortheestablishmentandperfectionofthecrustobodygeotectonicsth

简介：Since1993,thefirstauthorhasexpandedhisresearchongeotectonicsfromChinatothegloble,andhasputforwardhisownnewconceptsinglobaltectonics:TheoryofIntegratedPolygeneticGeotectonics.In2001,heandhiscoworkerspublishedtheirworks:twomapsandadetailedexplanatorynotebyGeologicalPublishingHouseofChina.

简介：从Dabie的南方盆的沙岩的由岩屑形成的模式(大别)orogenic带由于多重供应在早中间的侏罗记期间是复杂的。从降低中间的侏罗记的媒介粗糙的沙岩的由岩屑形成的作文，Huangshi(黄石)，表演三主要起源：再循环的ororgen，暴烈的弧(弧orogen)，和区别形式的作文的图和沙岩petrofacies的分析的Dickinson的底上的大陆人块。与稀少的出版paleocurrent数据，学习区域的大地构造的背景，和未出版的由岩屑形成的锆石年龄结合了数据，主要起源的位置如下被推断：在华东的沿海的orogenic带(圆块)作为再循环的orogen起源提供了岩屑；到北方的Dabieorogenic带(DOB)是暴烈的弧(弧orogen)的来源材料；并且大陆人块clasts从Yangtze地下室(UYB)的uplift是可能的(Jiangnan(江南)高举)。六个沉积周期在学习的节被认出，在武昌的(武昌)形成，并且五在Huajiahu(花家湖)形成。在免职期间，三主要起源起不同作用。量的petrofacies分析从每来源揭示了效果的不同变化，也就是说61.9%(周期我)→54.5%(周期III)→50%(周期IV)→57.9%(周期V)→14.3%(周期VI)，14.3%(周期我)→21.2%(周期III)→40%(周期IV)→36.8%(周期V)→14.3%(周期VI)，并且23.8%(骑车我)→24.2%(周期III)→10%(周期IV)→5.3%(周期V)→71.4%(周期VI)从圆块，DOB，和UYB分别地。结果证明(1)圆块在早侏罗记期间在可观的激活表现了，但是在中间的侏罗记变弱；(2)精力旺盛构造在中间的侏罗记开始的DOB高举；并且(3)UYB基本上在稳定从对中间的侏罗记早。