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简介:OnOctober27,2001,alargeearthquakewithMs6.0,namedtheYongshengearthquake,occurredalongtheJinshajiangsegmentofChenghaifaultinYongshengCounty,YunnanProvince.ItisthelargesteventtooccuralongtheChenghaifaultinthelast200years.Theseismo-geologicalsurveyshowsthattheseismogenicfault,whichistheJinshajiangsegmentofChenghalfault,takesleft-lateralstrike-slipasitsdominantmovementpattern.Accordingtodifferencesinverticalmotion,motiontime,landformsandscales,theChenhalfaultcanbedividedintoeightsegments.TheJinshajiangsegmenthasaverticaldislocationrateof0.4mm/a,farlowerthanthemeanrateoftheChenghaifault,about2.0mm/a.It'sdeducedthatthetwosidesofJinshajiangsegment'stuck'tightlyandhinderedthestrike-slipoftheChenghaifault.ThestrongearthquakedistributionbeforethiseventshowsthattheJinshajiangsegmentwasintheseismicgap.TheChenghaifault,asaboundaryoftectonicsub-blocks,makestheNorthwestYunnanblockandtheMiddleYunnanblockmoveclockwise,andtheirmarginsmoveoppositelyalongtheChenghalfault.InthemotionprocessoftheChenghaifault,structuralhindranceandtheseismicgapofstrongearthquakesarepropitioustotheconcentrationandaccumulationofstructurestress.Asaresult,theYongshengMs6.0earthquakeoccurred.TheSujiazhuang-ShangangfusegmentissimilartotheJinshajiangsegmentwithalowverticalmotionrateof0.3mm/aandintheseismicgap.Soit'spostulatedthatthesegmentmaybecomeanewstructurehindrance,andtheYongshengMs6.0earthquakemaytriggertheoccurrenceoffuturelargeearthquakesalongthissegment.
简介:Athree-dimensional(3-D)oceanmodeliscoupledwithatwo-dimensional(2-D)seaicemodel,torevisitanonlinearadvectionmechanism,oneofthemostimportantmesoscaleeddygenesismechanismsinthemarginalicezone.Two-dimensionaloceanmodelsimulationssuggestnonlinearadvectionmechanismismoreimportantwhenthewatergetsshallower.Insteadofconsideringtheoceanasbarotropicfluidinthe2-Doceanmodel,the3-Doceanmodelallowstheseaicetoaffectthecurrentdirectlyinthesurfacelayerviaocean-iceinteraction.Itisfoundthatbothmesoscaleeddyandseasurfaceelevationaresensitivetochangesinawaterdepthinthe3-Dsimulations.Theverticalprofileofacurrentvelocityin3-Dexperimentssuggeststhatwhenthewaterdepthgetsshallower,thecurrentmovefasterineachlayer,whichmakestheseasurfaceelevationbenearlyinverseproportionaltothewaterdepthwiththesamewindforcingduringthesametime.Itisalsofoundthatbecauseoftheverticalmotion,themagnitudeofvariationsintheseasurfaceelevationinthe3-Dsimulationsisverysmall,beingonly1%ofthechangeinthe2-Dsimulations.Anditseemstheverticalmotiontobetheessentialreasonforthedifferencesbetweenthe3-Dand2-Dexperiments.
简介:CloudresolvingWeatherResearchandForecasting(WRF)modelsimulationsareusedtoinvestigatetropicalcyclone(TC)genesisefficiencyinanenvironmentwithanearbottomvortex(EBV)andanenvironmentwithamid-levelvortex(EMV).Sensitivityexperimentsshowthatthegenesistimingdependsgreatlyoninitialvorticityverticalprofiles.Thelargertheinitialcolumnintegratedabsolutevorticity,thegreaterthegenesisefficiencyis.Giventhesamecolumnintegratedabsolutevorticity,abottomvortexhashighergenesisefficiencythanamid-levelvortex.Acommonfeatureamongtheseexperimentsistheformationofamid-levelvorticitymaximumpriortoTCgenesisirrespectivewheretheinitialvorticitymaximumlocates.BoththeEMVandEBVscenariossharethefollowingdevelopmentcharacteristics:1)atransitionfromnon-organizedcumulus-scale(~5km)convectivecellsintoanorganizedmeso-vortex-scale(~50to100km)systemthroughupscalecascadeprocesses,2)theestablishmentofanearlysaturatedaircolumnpriortoarapiddropofthecentralminimumpressure,and3)amultipleconvective-stratiformphasetransition.Agenesisefficiencyindex(GEI)isformulatedthatincludesthefollowingfactors:initialcolumnintegratedabsolutevorticity,vorticityattopoftheboundarylayerandverticallyintegratedrelativehumidity.ThecalculatedGEIreflectswellthesimulatedgenesisefficiencyandthusmaybeusedtoestimatehowfastatropicaldisturbancedevelopsintoaTC.
简介:LaoyalingstratiformcopperdcpositislocatcdlokmeastofTonglingcity,AnhuiProvlncc.ItisatypicalstratiformdcpositinthclowcrandmiddlearcaofYangtzorivcr,farfromplutonicrocksandhostedinPcrmiansilicalites.Thcorcbodicsoccuraslaycr,likelayerandlcnsc,whichhavethesameoccurrcnceasstrataandbotliofthemwcrefoldcd.Ore
简介:<正>XianghualingorefieldislocatedinLingwuCounty,HunanProvince.Itliesonthein-tersectionofpoly-setstructuresandbelongstononferrousrare-polymetalminetalizationse-riesrelatedtothecrust-origingraniteinactivationregion.Thestrataoftheorefieldin-volvesCambrian(∈),Devonian(D)andCarboniferous(C),inwhichCambrianepimeta-morphicsandstone,D2tsandstoneandD2q-D(3x)dolomiteareconsidedastheoresource-bedoftheoredeposit.Severalhigh-replacementalstocks,whichlieabovethehiddengranitebatholithwithNNWtrending,intrudealongtheintersectionofNWandNEtrendingfaults.
简介:TheBashansuperlargebariumdeposit(withcritetype)islocatedinnortheasternSiehuanProvince.GcotcctonicallyitissituatcdinthcsoutbernpartoftheDabashangcodomespetcm’Centra1Chinadiwarcgion,onthcnorthcrnsideoftheSouthDabashanfracture.BariumbedsarehostedbythcLowcrCambrianLujiapingFormation.Themetallogeniczonec
简介:ShanjiadistrictofeastcrnHcbciProvinccislocatcdinsouthcrnlimbofEWtrcndingYanshangeodomechain,whichbe1ongstoHchuaidiwasystcmofNorthC!1inadiwarcgion.Inthestudiedarca,morethanlogolddcposits(occurrenccs)wcrcdistributed,includingShanjia,Xinglonggou,WangjiagouandWcizigougo1dMincs’Archcanmctamorphicrocksare
简介:0vcrl00pyrophylliteoccurrcnccs(dcposits,orcsp0tsandmincralisedsp0ts)havebeenfuul1dinChina-Am0ngthemab0ut90%arerelatcdtotbeacti0nofv0lcanicgas-1iquidandaccountf0rabout87Koftbcprovcdrcserves.ManylargcandsuperlarScpyr0phy1litedcp0sitsbclongtothistype.Thercf0re,pyr0phyllitedep0sitsofv0lcanicgas-1iquida1
简介:RareelementmineralizedgranitesoftheYanshanperiodinSouthernChinaarecharacterizedbyhighcontentsofSiO2,Na2O,O,K2O,andFandareenrichedinNb,Ta,REE,W,Sn,BeandLi.Opinionsdif-feredoverwhethertheyareofmetasomaticormagmaticorigin.Inthispaper,wepresentresultsofastudyonmeltandfluidinclusionsintopaz-albitefeldspargranitefromLimoNb-Ta-W-Sngraniteand414Ta-Lialbitegranite.Ourdata,whichcomefrom15mineralizedgranites,providestrongsupportmagmaticorigin.Meltinclusionsarerecognizedinbothtopazandquartz,andareassociatedwithprimarygas-richinclusions.CrystallitesofaNb(Ta)-bearingmineralandcassiteritearealsocommonlypresentasinclusionsinthetopaz.Multiphase(melt+fluid)inclusionsareobservedinsomequartzfromgranitesandgranite-relatedpegmatite.Meltinclusionsstarttomeltatatemperatureofapproximately540℃intopazand650℃inquartz.Finalhomogenzationtemperatureis700-900℃inquartz,700-800℃intopazand440—550℃forpri
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简介:有细密纹理的碳酸盐岩石,它广泛地发生在始新世在Shulu的阶层下垂,Bohai海湾盆,诺思中国,代表一座异乎寻常的、有细密纹理的碳酸盐水库。然而,以前的研究忽略了岩相部件和他们的形成机制的复杂性。有细密纹理的碳酸盐岩石是烃在形成并且聚在一起的典型水库。这些岩石的性质的更好的理解为评估异乎寻常的、有细密纹理的碳酸盐水库的质量是极其重要的。各种各样的岩相部件与petrographic观察和碳同位素分析的联合在这研究被区别。这些有细密纹理的碳酸盐岩石包括源自陆地,源於生物并且diagenetic材料。源自陆地的输入和生物学上导致的降水是在湖的材料的主要来源。五张岩相基于沉积特征(核心和薄节)和矿物学的数据的观察被识别:(1)像纹泥的把压成薄片的calcilutite,(2)分级把压成薄片的calcilutite,(3)interlaminatedcalcisiltitecalcilutite,(4)巨大的calcilutite,并且(5)巨大的calcisiltite-calcarenite。他们的起源被各种各样的岩相部件记录,它被物理、化学、生物的过程的相互作用控制。这研究显示基岩的岩性学是控制碳酸盐累积的关键因素。tectonics和气候能影响捱过和岩相的类型。主要生产率控制了endogenic方解石的降水。这些因素联合决定在Shulu积累了的丰富的有细密纹理的碳酸盐岩石下垂。
简介:Withanexploitationliistoryofmorctban500years,LaocliangorcdepositinLancliang,Yunnanisaparticularlylarge(possiblysuperlarge)oneofAg,Pb,Th,Cu,S,Au,etc.TectoniCally,itis1ocatedalmostinthesouthcmendofBaolangeodomespetemofWcsternYunnandiwaregion(ChenGuoda,1977)’StrataexposedintheminjngrraionareDevonisnSgn
简介:ThisstudyexaminestheseasonalvariationsoftropicalcyclogenesisovertheSouthChinaSea(SCS)usingagenesispotential(GP)indexdevelopedbyEmanuelandNolan.Howdifferentenvironmentalfactors(includinglow-levelvorticity,mid-levelrelativehumidity,verticalwindshear,andpotentialintensity)contributetothesevariationsisinvestigated.CompositeanomaliesoftheGPindexareproducedforthesummerandwintermonsoonsseparately.ThesecompositesreplicatetheobservedseasonalvariationsoftheobservedfrequencyandlocationoftropicalcyclogenesisovertheSCS.Thedegreeofcontributionbyeachfactorindifferentregionsisdeterminedquantitativelybyproducingcompositesofmodifiedindicesinwhichonlyoneofthecontributingfactorsvaries,withtheotherssettoclimatology.OverthenorthernSCS,potentialintensitymakesthelargestcontributionstotheseasonalvariationsintropicalcyclogenesis.OverthesouthernSCS,thelow-levelrelativevorticityplaystheprimaryroleintheseasonalmodulationoftropicalcyclone(TC)genesisfrequency,andtheverticalwindshearplaysthesecondaryrole.ThermodynamicfactorsplaymoreimportantrolesfortheseasonalvariationsintropicalcyclogenesisoverthenorthernSCS,whiledynamicfactorsaremoreimportantintheseasonalmodulationofTCgenesisfrequencyoverthesouthernSCS.