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简介：Inthispaper,researchofaftershockmechanismsisreviewed,includingheterogeneityofmediumandstress,mechanicalloading,fluidintrusionandstresscorrosion,andratestatedependence.Previousstudieshaveindicatedthattheheterogeneityofmediaandstressisthebasicpremiseofaftershocksgenerated.Fromthepointviewofmechanics,transientcreepandafterslipcanexplainthedecayofaftershocksinashorttimeafteramainshockandtherelaxationofstresstendstointerpretthecharacteristicsoflong-termaftershocks.Fluidintrusionandstresscorrosioncontroltheevolutionprocessoftheaftershocksundercertainconditions.Theinteractionbetweenthefaultsperturbedbythemainshockalwaysexistsduringtheaftershockactivities.Allkindsofmodelsandthetheorieswanttocomplywiththetwobasicpower-lawrelationships---theG-RlawandOmorilawtosomeextent.

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简介：ＤｅｆｏｒｍａｔｉｏｎｄａｔｕｍｉｎｓｏｕｒｃｅｍｅｃｈａｎｉｓｍｉｎｖｅｒｓｉｏｎＳＨＯＵ－ＷＥＮＧＯＮＧ（巩守文，ＱＩＮＧ－ＬＩＡＮＧＷＡＮＧ（王庆良），ＹＩ－ＱＩＮＧＺＨＵ（祝意青）ａｎｄＢＩＮＧＣＨＥＮ（陈兵）（ＳｅｃｏｎｄＣｒｕｓｔａｌＤｅ...

简介：Ｓｅｉｓｍｏｇｅｎｉｃ　ｍｅｃｈａｎｉｓｍ　ｏｆ　ｔｈｅ　Ｌａｎｃａｎｇ　ａｎｄ　Ｇｅｎｇｍａ　ｅａｒｔｈｑｕａｋｅｓ（俞维贤）（周瑞琦）（候学英）（周光全）ＳｅｉｓｍｏｇｅｎｉｃｍｅｃｈａｎｉｓｍｏｆｔｈｅＬａｎｃａｎｇａｎｄＧｅｎｇｍａｅａｒｔｈ...

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简介：试用被坝所围住的水从2008年9月27日在三座峡水库被继续。在Hefeng有强壮的变丑和失败()山崩当水库水水平从173m的高度下降了时。它显示变丑是仔细与水库水变化有关。为这个原因，在变丑的水库水的效果被学习，拿象在这篇文章的一个例子的Hefeng山崩。首先，强壮的变丑区域的地质的特征和变丑状况被分析透露内在的因素和在水的条件下面的变丑的模式铺平变化。第二，山崩的稳定性在升起并且下降的过程，和在水库水水平变化和山崩变丑之间的相应关系期间被计算进一步被识别。最后，渗出物领域和在井的线下面的山崩身体的力量条件被分析揭示水库水的效果。而且，为更好可渗透的水库山崩，在水库水升起期间，渗出物力量的有利效果削弱相反的效果，这能被结束高举强迫水库水升起稳定性上的小效果，和没有变丑被引起了；但是在下降水库期间流水，渗出物力量的相反的效果在uplift力量的相反的效果上被附加，它引起稳定性戏剧性地减少并且在山崩前面导致累积身体的失败。

简介：ApossiblemechanismisputforwardinthispaperforElNinoeventsfromtheviewpointofplatetec-tonicsandoceanicgeology.Anumberofthedataarecitedtoillustratetheviewsthatsea-bottomvolcanicac-tivitiesandhotspringsmaycauseElNinoevents.

简介：HAB(harmfulalgalbloom)isaseriousmarineecologicaldisaster.Uptonowthereisnodefiniteconclusionaboutitsmechanismofoccurrence.TheobservationresultsshowthattheHABbreakoutintheXiangshanBaywasmainlycausedbyphysicalconvergencecapacity,andthebreakoutprocesshadnodirectrelationtoeutrophication.AsanewideaitisthoughtthattheprocessoftheHABbreakoutismainlyaphysicalconvergenceoraccumulationprocessinsomeareas.AhypothesisaboutdynamicmechanismoftheHABappearingintheareaofftheChangjiangEstuaryisputforwardaccordingtohydrologyandtopographyandthepastwork,andabreakthroughisexpectedtobemadefordoingfurtherresearch.

简介：1,209earthquakesoccurredinXianyou,FujianfromAugust4,2010toOctober4,2013.ThelargestearthquakewasML5.0onSeptember4,2013.InordertostudytheXianyouearthquakesequenceandunderstandthecausativestructureandstressfieldofXianyou,thefocalmechanismsolutionsofsixearthquakes(ML>3.5)intheXianyouearthquakesequencearecalculatedusingthebroadbanddigitaldataoftheFujianSeismicNetworkwiththeseismicmomenttensorinversemethod.Theresultsshowthatthefocalfaultsofthesixearthquakesaresimilar,whichareallstrike-slipfaultsstrikingtothenorthwestwithhighdipangles.ThedirectionoftheprincipalcompressivestressaxesisnearSN,whichisdifferentfromthestressfieldofFujianregion.TheXianyouearthquakesequencemayhavebeeninducedbythestressadjustmentaftertheimpoundmentofJinzhongreservoir.

简介：Forskarntypedeposits,therearetwokindsofskarns,skarnformedbyfiltrating-diffusingmetasomatismandveinskarnformedbyfilling.Theveinskarn,discussedthispaperandconsideredtobemagmaticgenesis,ischaracterizedby:(1)occurringasveinwithdistinctboundarieswithcountryrocks,yetjustthesameeveninmarbleeasytobereplaced;(2)composedofamineralassemblagesimi-lartothatofgranite,containingpegmatiteaswellascoarseskarnmineralpockets,andsometimestran-sitedwithdikerocks;(3)clearcrystallinefeatureofdeposition;(4)sideronintietexture;(5)showingvesicular,bean-likeandflowstructures;(6)verycommonliquidimmiscibility;(7)verticalzoningofgravitationaldifferentiationcausedbyvolatileconcentrationupwards;(8)associatedandtransitedwithiron-copperorebodiesofmagmaticgenesisandtungsten-bearingquartzveinsofsilicatemagmaticgene-sisrichinvolatile;(9)meltinclusions.Twooriginsofskammagma,originatedbyassimilationofsilicatemagmaatitsemplacem

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简介：Withhypermediatechnologythestructureofapublicationcanbere-arrangedtoaccommodatemoreeasycognitionoftheideaandconceptbylinkingtheconceptswhicharerepresentedbydifferentmediaformsintoanintegratedconcept.Essentially,multimediaelectronicatlasisakindofelectronicpublication,whichhasmanycommoncharacterswithordinaryCD-ROMpublications.Forthedeeperexplorationofelectronicatlasitisveryimportanttounderstandtheinternalandgeneralstructureofthenewmediastructure.Theaimofthispaperistodiscusstheinternalstructureofmultimediaelectronicatlasasawholebyapplyingthemethodologyoflinguistics.

简介：ＴＨＥＣＩＳＫＭＥＣＨＡＮＩＳＭＡＮＤＴＨＥＩＮＥＲＴＩＡＬＧＲＡＶＩＴＡＴＩＯＮＡＬＷＡＶＥＳＩＮＳＨＥＡＲＦＬＯＷＷｕＨｏｎｇ（吴洪）；ＸｉａＹｏｕｌｏｎｇ（夏友龙）ａｎｄＺｈｅｎｇＺｕｇｕａｎｇ（郑祖光）（ＢｅｉｊｉｎｇＩｎｓｔｉｔｕｔｅｏｆＭ...

简介：TheQiangtangbasinislocatedbetweenKekexili-JingshajiangsuturebeltandBangong-Lujiangsuturebelt,andisdividedintothenorthpartandsouthpartbythecentralupliftthathasnocropoutofMesozoicstrata.WhentheJinshajiangOceanwasclosed,thesubductingplatewassubductedsouthward.InthecentralpartoftheQiangtangbasin,thecushioningeffectoftheasthenosphereresultedinthethermaldomingofthemantleandsubsequentlarge-scaleanatexis.Mantlesourcematerialsandantecticmaterialswereupwelledandextrudedintothemiddlecrust,leadingtothethickeningofthemiddlecrustandtheheatingandweakeningofthemiddletouppercrust,andresultingintherapiddeformation(detachment)andtectonicerosion,andintheisostaticupliftingandtheformationofmetamorphiccorecomplex.Theupwellingofanatecticmaterialswouldfurtherenhancethebuoyantrepercussion,whichwouldcombinewiththesidestressduefromextrusioninresultingintheformationofanextensionalstressfield.Theextensionalstructureanddetachmentfaultareformedundertheinfluenceofthelosingstabilizedgravitation.Inthedeformationareainboththeupperpartandthelowerpart,anextensionaldepositionareawouldbeformed,andthisisthegenerationofanewbasin.Themetamorphiccorecomplexofthecentralupliftiscomprisedofgneiss,whichisitselfoverlainbynon-metamorphictoweaklymetamorphiccoveringstrataintersectedbyfaults.

简介：Beforeintruding,primarymagmashaveundergoneliquationandpartialcrystallizationatdepth;asaresultthemagmasarepartitionedintobarrenmagma,ore-bearingmagma,ore-richmagmaandoremagma,whichthenascendandareinjectedintothepresentlocationsonceormultipletimes,thusformingoredeposits.Theabove-mentionedmineralizingprocessisknownasdeep-seatedmagmaticliquation-injectionmineralization.Thevolumeofthebarrenmagmaisgenerallymuchlargerthanthoseoftheore-bearingmagma,ore-richmagmaandoremagma.Intheascendingprocess,mostofthebarrenmagmaintrudesintodifferentlocationsoroutpoursontothegroundsurface,formingintrusionsorlavaflows.Therestbarrenmagma,ore-bearingmagma,ore-richmagmaandoremagmamayeithermultipletimesinjectintothesamespaceinwhichrocksandoresareformedorseparatelyinjectintodifferentspacesinwhichrocksandoresareformed.Theintrusionscontainingsuchdeep-seatedmagmaticliquation-injectiondepositshaveamuchsmallervolume,greaterorepotentialandhigheroregradethanthatofin-situmagmaticliquationdeposits.Consequentlythismineralizingprocessresultsintheformationoflargedepositsinsmallintrusions.

简介：Inthispaper,therelationshipsoftheplungesandazimuthsofTandPaxesversusthestrikes,dips,andrakesoftwoseismicnodalplaneswerederivedtoprovidereferenceforearthquakeresearchers.TheindependenceoftheplungesandazimuthsofT,B,andPaxesinfocalmechanismsolutionwasdiscussed,anditwasconcludedthatthreeparameters,i.e.,theazimuthsofT,BandPaxes,arecompletelyindependent.ThefocalmechanismsolutionrepresentationbasedonEulerrotationwasintroduced,usingthreeEuleranglesinplaceoftheplungesandazimuthsofT,B,andPaxes,andthreefocalmechanismsolutionrepresentationswerebrieflycomparedandanalyzedinrespectofaccuracyonthebasisoftheassumptionofrounding;itwasconcludedthattheEuleranglerepresentationhasbetteraccuracy,comparedwiththeazimuthrepresentationandthetraditionalrepresentationwithT,B,andPaxes.

简介：1IntroductionMechanismsoftheearth’shardcrust(crustobody)movementhavebeenhypothesizeda8tide,expansionandcontractionofthccarth,mantleconvection,rotationoftheearth,etc’,whicharenotcloselyreasoneddespiteofthesupportofsomegeologica1facts’Anothcrhypothesis-themantlecreep-flowandgeothermalencrgyconccrvatio

简介：A2-Dglobalchemistry-transportmodelissetupinthispaper.Themodelsimulatestheatmosphericozonedistributionswellwithspecifieddynamicalconditions.Theanalysisofozonevariationmechanismshowsthatozoneischemicallyinquasi-equilibriumexceptforthepolarnightregionwherethevariationofozoneconcentrationisunderthecontrolofdynamicalprocesses,thattheoxygenatomswhichproduceozonearemainlyprovidedbythephotolysisofO2intheupperstratosphereandbythephotolysisofNO2inthelowerstratosphereandthetroposphere.andthattheozoneisdestroyedmainlybyNOx:thereactionsbetweenNOxandO3andtheoddoxygencyclecontribute80%tomorethan90%oftheozonedestruction.