简介:Inthispaper,researchofaftershockmechanismsisreviewed,includingheterogeneityofmediumandstress,mechanicalloading,fluidintrusionandstresscorrosion,andratestatedependence.Previousstudieshaveindicatedthattheheterogeneityofmediaandstressisthebasicpremiseofaftershocksgenerated.Fromthepointviewofmechanics,transientcreepandafterslipcanexplainthedecayofaftershocksinashorttimeafteramainshockandtherelaxationofstresstendstointerpretthecharacteristicsoflong-termaftershocks.Fluidintrusionandstresscorrosioncontroltheevolutionprocessoftheaftershocksundercertainconditions.Theinteractionbetweenthefaultsperturbedbythemainshockalwaysexistsduringtheaftershockactivities.Allkindsofmodelsandthetheorieswanttocomplywiththetwobasicpower-lawrelationships---theG-RlawandOmorilawtosomeextent.
简介:Seismogenic mechanism of the Lancang and Gengma earthquakes(俞维贤)(周瑞琦)(候学英)(周光全)SeismogenicmechanismoftheLancangandGengmaearth...
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
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.