简介:西方的云南位于在Gondwana和劳亚古大陆之间的一个巨大的Tethyserogenic地区以内。联系威尔森orogenic周期的Magmatic活动记录证明板在这个区域传播的原因可能与亚披风羽毛有关。Tectonics,地球物理,沉积阶层,岩石圈的构造进化和另外的研究结果显示为在韦斯特云南的披风羽毛magmatic活动有地质的证据。断层摄影术也支持在韦斯特云南红河差错和一根upwelling披风羽毛附近有一个subducting平板的想法。这里,我们的研究为upwelling披风羽毛介绍地震证据,它是在韦斯特云南导致subducting平板的一个主要原因。分析基于变换的compressional-to-shear(P-to-S)地震阶段,在四川云南地震网络在地震计上记录了车站,并且在410-km和660-km断绝上,以及在叠的CCP的三节上做了研究。
简介:有一条早侏罗记有四足的ornithischian恐龙的多重、保存得很好的trackways的一个大轨道地点是从亚洲的象Moyenisauripus一样trackways的第一份报告,此处命名的Shenmuichnusyoungteilhardorum。轨道在Shenmu县在Fuxian形成发生在一个碎屑状的河的序列,Shaanxi省,在象Sinoichnites的发现地点的一样的一般区域,第一条恐龙轨道从中国报导了。基于尺寸和形态学,Sinoichnites,现在被失去,也代表ornithischian,是可能的。Shenmuichnusyoungteilhardorumtrackways表演保藏的二个模式:第一与沉积边界,代表更深的磁道导致象Deltapodus一样磁道与模糊的足位踪迹和亚通报手踪迹,第二生产象Moyenosauripus一样磁道,与在足和手的清楚的有三指、有五指的位踪迹分别地。因此Shenmutrackways戏在解决从亚洲,非洲和欧洲包围Sinoichnites,Moyenosauripus,说出的Deltapodus(Ravatichnus)和未命名的trackways的名称的全球性重要的ichnotaxonomic问题的一个关键角色。另外,他们在早中生代在paleogeographical和有四足的ornithischians的paleoecological分发上打开重要的灯。轨道地点是主要挖掘的焦点从他们的原来的遥远的地点把trackways转移到新Shenmu博物馆,在Shenmu城市里。在表明和Shenmuichnus和植物石块证据,Anomoepus,Grallator和Deltapodusmorphotype为tracksite建议早侏罗记年龄的区域的另外的tracksites。
简介:TheDevoniansuccessioninSouthChinaiswell-knownforitscompletedevelopment,vari-fiedsedimentarytypes,remarkablelithofaciesvariationandabundantmineralresources.TheSouthChinaplatewasformedbythecollisionandcollageoftheYangtzeplateandtheCathaysianplate.ThecollisionbeganapproximatelyattheJinningianstageandthecollagewasnotfinalizeduntiltheGuangxianmovement.ItwasontheSouthChinaplatewithasomewhatdifferentnatureofthebasementthattheDevoniandepositionformed.
简介:AmarinestratigraphicsequenceacrossthePliocene/Pleistoceneboundaryhasbeenfoundinthenorth-erncontinentalshelfoftheSouthChinaSea.ThemarineQuaternarydepositsintheYinggehaiBasinmayex-ceed2,000minthickness,probablyprovidingthebestsectionforstudyingthelowerboundaryofthemarinePleistoceneinSouthChina.TheverticalsuccessionwithplanktonicforaminifersandnannofossilsrevealedinboreholesinthebasinhasbeenwellcorrelatedwiththatintheinternationalstratotypesectionofthePliocene/PleistoceneboundaryatVrica,Italy,resultingintheacquirementofabiostratigraphicboundaryat1.64Ma.Thisboundary,however,doesnotcoincidewithanyprominentlithologicalpalaeoenvironmentalchangesinthestudyareaandcanhardlybeusedingeologicalpractice.Thereare,incontrast,significantchangesatthelevelofLADofGloborotaliamulticameratasensulatolocatedbelowtheabove-mentionedboundary.Thepercentageofplanktonicforaminifersinthetotalpopulationandpreservationofforaminiferaltestsdisplaygreatchangesatthislevelcorrespondingtoaclearonlapontheseismicprofilesandindicatingadepositionalhiatusatca.2.0-2.5Ma.SincethelevelcanbewidelytracedinthePearlRiverMouthBasinandtheBeibuGulfBasinandwellcorrespondswiththemarkeddepositionalenvironmentalchangesrecordedinthewestPacificandotherregions,itisrecommendedthatthePlio/PleistoceneboundarybedrawnatthelevelofGr.multicameratasensulatoLAD,roughlyconcurrentwiththeGauss/Matuyamaturn.
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简介:Inestuarineandcoastalareas,theseabedisinaconstantprocessofdynamicchangeundermarineconditions.Seabedsedimenterosionandresuspensionareimportantprocessesthatsafelycontrolthegeologicalenvironment.FieldtripodobservationsconductedintheJiaozhouBayinChinaarereported,toinvestigatetheeffectsofhydrodynamicconditionsontheerosionandresuspensionprocessesoftheseabed.Theobservationalresultsshowthatthemaximumshearstresscreatedbytidalcurrentscanreach0.35N/m~2,whichishigherthanthewave-inducedshearstressduringfairweatherconditions.Aseabederosionfrequentlyoccursduringthefloodtide,whereasaseabeddepositionoccursduringebbtide.WavescanproduceabottomshearstressapproximatelyequivalenttothatinducedbycurrentswhenthelocalwindreachesForce4withaspeedof5m/s.Whenthewindreaches7m/sandthesignificantwaveheightreaches26cm,wavesplayamoresignificantrolethancurrentsinthedynamicprocessesoftheseabedsedimentresuspensionandleadtoahighvalueofturbiditythatisapproximatelytwotoeighttimeshigherthanthatinfairweather.Theseanalysesclearlyillustratethatperiodiccurrent-inducedsedimenterosionandresuspensionaredominantinfairweather,whereasepisodichighwavesareresponsibleforsignificantsedimentresuspension.AdditionalworkisneededtoestablishamorethoroughunderstandingofthemechanismsofsedimentdynamicsintheJiaozhouBay.
简介:Itisaverycomplicatedproblemtoestimateevapotranspiration(ET)overalargeareaoflandsurface.Inthispaper,theevapotranspirationestimationmodelsfordensevegetationandbaresoilarepresented,basedontheinformationofparameterslikevegetationcover-degreeandsurfacealbedo.Combinedwithvegetationcover-degreedata,amodelforregionalevapotranspirationestimationovertheheterogeneouslandscapeisderived.ThroughacasestudyusingremotesensingdataoverNorthwestChina,theaccuracyofthemodelforregionalevapotranspirationestimationischecked.Theresultshowsthattheaccuracyofthemodelissatisfactory.ThefeaturesofevapotranspirationoverNorthwestChinaarealsodiscussedwiththeapplicationofthemodel.
简介:Thebasin-and-rangeareaineasternNorthChinaisknownforfrequentoccurrenceofearthquakes,theirgreatmagnitudesandheavylossestherebyincurred.Seismicstudiesinthepastusuallyemphasizedtheintersections,inflexionsandbranchesofthefaults.However,theintensitiesofmanygreatearthquakesinthisareadonotshowlineardistribution,andtheepicentersarehorizontallydispersedatcertaindepthsinsteadofalongthestrikeoffaults.Basedonthesub-mantleplumestudiesmadebyauthorsinthepastdecade,itisthoughtthatthereexistsanupliftedsub-mantleplumeunderthefaultdepressionareainNorthChina.Theupliftingandintrusionofmantlematerialscausedtheuppercrusttobefaulted,whilelow-velocityandhigh-velocitylayersarealternativelydistributedinthemiddlecrustundertheinfluenceofthemantleandthelowercrust.Themiddleandlowercrustmaterialsweredetachedfromthetopofthesubmantleplumetothesurroundingswhilethesub-mantleplumematerialsweredetachedoutward.Whenthedetachedmiddleandlowercrustcometotheboundaryoffaultbasinsintheuppercrust,theywillbeobstructedbytheorogeniczoneandthedetachmentwillgoslower.Theshearingbetweenthemwillcausethestresstoaccumulateandreleasealternatively,sothatearthquakesoccurredfrequentlyintheareasofsub-mantleplumeanditssurroundings.
简介:ThemeasurementsbyusingADCP(500KH)andCTDweremadeduringAugust2000inthesouth(37°55'N,120°25'E)oftheBohaiSea,wherethewaterdepthwasabout16.5m.Thedataofhorizontalvelocitywithsamplingintervalof2minin7layerswereobtained.Thepowerspectrumanalysisofthesedataindicatesthatthereareveryenergeticinfragravitywaveswithaperiodofabout6min.Thecoherencespectrumanalysisandtheanalysisoftemporalvariationofshearshowthattheseinfragravitywavesaremainlythefreewavemodel(propertiesofedgewaves),inthemeantimetheypossesssomecharacteristicsofinternalwaves,whicharelikelyduetothedistinctivemarineenvironmentinthisarea.Itisspeculatedonthattheinstabilityprocesses(chieflyshearinstability)ofshearedstratifiedtidalflowowingtotheeffectofsea-floorslopeinthecoastalareamightbethemainmechanismgeneratingtheseinfragravitywaves.
简介:西北中国包括XinjiangUgyur自治区域,Qinghai省,Gansu省,NingxiaHui自治区域和Shaanxi省,盖住308x10~4km~2。它位于温暖适度的地区,气候干旱或半干旱。降水是很少见的,但是蒸发极其高。气候是干燥的,水资源是缺乏的,theeco环境是易碎的,并且水资源的分发是不平的,降水是唯一的输入,并且蒸发是内陆河,和猛冲里的唯一的输出,在这个区域,与对方一起的表水和地下水变化为多次,它有益于水资源的存储和利用。在这个区域的平均降水是232公里,全部的降水数量是7003x10~8m~3/a,表水资源是1891x10~8m~3/a,全部的自然地下水资源是1150x10~8m~3/a,全部的有效水分资源是438x10~8m~3/a,和全部的水资源是8m~3/a和人均的水资源是的1996x10~2278m~3/a。整个区域的水资源是5.94x10~4m~3/(a.km~2),仅仅是在中国的五分之一个平均值。现在,有效水分资源是876x10~8m~3/a,地下水在之中是贴近的130x10~8m~3/a。
简介:Basedonacurrentfogdetectiontheory,amultibandthresholdmethodforMODISdatawasputforwardtodetectdaytimefogintheSouthChinaSea.ItusedBands1,2,18,20and31ofMODISdatatoseparatefogfromthecloudandtheseasurface.Thedigitaldetectionindexeswereasfollows.IfRB1<20%,RB2<20%andRB1>RB2,thepixelwasidentifiedtobetheseasurface.IfRB1>55%,RB2>55%andTB31<273K,thepixelwasidentifiedtobeamiddle-andhigh-levelcloud.IfIFC>20,thepixelwasclassifiedtobeseafog.ThemethodwasverifiedwithseafogdataobservedfromthecoastalregionofGuangdongduringJanuary-April2011.Outofthe13samplesofsatellitedetection,ninewereconsistentwiththesurfaceobservations,threewereidentifiedtobelow-levelthecloudaccordingtothesatellitedetectionbutfogaccordingtothesurfaceobservations,andonlyonesamplewasidentifiedtobetheoceansurfacebythesatellitedetectionbutfogbythesurfaceobservations.BecausetheMODISdatacannotpenetratethecloudorfog,themodelwasdesignedforasinglefieldofviewwhichhadonlyonelayerofcloudorfog.Itcanaccuratelydistinguishfogwhichisnotcoveredbythecloud,butitidentifiesfogascloudiftheformeriscoveredbyacloud.Generallyspeaking,themodeliseffectiveandfeasible.
简介:用先进研究WRF(ARWWRF)当模特儿并且Gridpoint统计插值(GSI)三维的变化分析(3DVAR)系统,吸收ATOVS的影响(先进初学者运作垂直更健全)通过原型社区放射的转移模型(pCRTM)的发光在预报在2005年6月20-21日在中国的东南发生在中央广东省上的重暴风雨上被评估。为这个盒子的一双比较实验(NODA和DA)与多重配置被进行,包括嵌套有4-km和12-km格子距离的领域。结果证明由通过数据吸收改变起始的条件,有偶极子的结构的一个修改分叉和潮湿领域与西南东北取向被加到雨线的轴。当一口西南的低级喷气(LLJ)带的更多的潮湿在Longmen的天文台车站附近被集成进雨线的东北部分时,,潮湿静电干扰精力(MSE)的振幅在中间的层次在底层实质地增加了,导致在在500hPa和850hPa之间的MSE扩大差别;空气变得更不稳定。因而,对流降雨在Longmen车站附近在省的东北部分增加了,它与降雨的观察分发一致。
简介:在空中的gravimetry世界地球物理的探索的历史上是重要跳跃和革新。中国在空中的严肃的第一测试在Bohai海的西方、南部的部分的向陆近海的过渡区域的地质的调查在地质学成功、有效。基于在空中的严肃数据,并且联合以前的扎根的严肃,地震、钻的数据等等,我们由前面、反的方法执行了地质的解释。在空中的Bouguer严肃异例是清楚的,破裂解释是可靠的,并且主要地质的接口的倒置深度是相对精确的结果表演。这在空中的严肃地质的调查不仅在向陆近海的过渡区域充满了探索差距,并且认识到在海和陆地之间的地质、构造的连接,而且发现了四个本地严肃异例,11破裂并且三下垂或subsags等等。没被地面状况限制的在空中的gravimetry的好地质的效果证明它能在象山脉那样的复杂地面相法区域的探索作为一个新地球物理的方法被服务,丛林,沙漠,沼泽地,向陆近海的过渡区域等等,并且以后在中国有广泛的申请前景。