简介：Recentandpaleo-submarinelandslidesarewidelydistributedwithinstrataindeep-waterareasalongcontinentalslopes,uplifts,andcarbonateplatformsonthenorthcontinentalmarginoftheSouthChinaSea(SCS).Inthispaper,high-resolution3Dseismicdataandmultibeamdatabasedonseismicsedimentologyandgeomorphologyareemployedtoassistinidentifyingsubmarinelandslides.Inaddition,depositionmodelsareproposedthatarebasedonspecificgeologicalstructuresandfeatures,andwhichillustratethelocalstressfieldoverentiresubmarinelandslidesindeep-waterareasoftheSCS.TheSCSisoneofthelargestfluvialsedimentsinksinenclosedorsemi-enclosedmarginalseasworldwide.Itthereforeprovidesasetofpreconditionsfortheformationofsubmarinelandslides,includingrapidsedimentaccumulation,formationofgashydrates,andfluidoverpressure.Anewconceptinvolvingtemporalandspatialanalysesistestedtoconstructarelationshipbetweensubmarinelandslidesanddifferenttimescaletriggermechanisms,andthreemechanismsarediscussedinthecontextofspatialscaleandtemporalfrequency:evolutionofslopegradientandoverpressure,globalenvironmentalchanges,andtectonicevents.Submarinelandslidesthataretriggeredbytectoniceventsarethelargestbutoccurlessfrequently,whilesubmarinelandslidestriggeredbythecombinationofslopegradientandoverpressureevolutionarethesmallestbutmostfrequentlyoccurringevents.Insummary,analysisshowsthattheformationofsubmarinelandslidesisacomplexprocessinvolvingtheoperationofdifferentfactorsonvarioustimescales.

简介：从在诺思中国上的2010-14的严重天气报告和合成雷达反射率数据被用来分析严重的对流的风(SCW)的分发事件和他们雷达反射率的组织上的模式。为SCW事件的六个组织上的模式(并且他们的比例)簇房间(35.4%)，嚎啕线(18.4%)，非线性形状的系统(17.8%)，破线(11.6%)，单个房间(1.2%)，和弓回应(0.5%)。为嚎啕线和破线的山峰月是6月，而它是为另外的四个模式的7月。SCW事件的最高的数字在山上，它通常与簇房间的瓦解的系统被联系。相反，与线性系统联系的SCW主要在平原上发生了，在车站每年记录了不到一个SCW事件的一般水准的地方。有与非线性形状的系统联系的SCW的高频率的区域也经历了与嚎啕线联系的许多SCW事件。对流可得到的势能的价值，能使沉淀的水，0-3-km砍，并且0-6-km砍，比在山上在平原上是可论证地更大的，它在SCW事件的组织上的模式上有明显的效果。因此，地形学可以是在为在诺思中国上的SCW事件的组织上的模式的一个重要因素。

简介：Mid-latitudeair-seainteractionisanimportanttopicthatattractsaconsiderableamountofresearchinterest.TheKuroshioExtension（KE）isoneofthemainwesternboundarycurrentsandplaysacriticalroleinthemid-latitudeatmosphericcirculation.ThispaperusestheNCEP/NCARreanalysisandHadleyseasurfacetemperaturedatasetstoinvestigatetheinfluenceofoceanicfrontsintheKEregiononsurfaceairtemperatureinNorthAmericaovertheperiod1949–2014.AsignificantcorrelationwasfoundbetweentheKEfrontintensityandthetemperaturesoverNorthAmericainautumnandwinter.Astrong（weak）KEfrontanomalyinautumnisassociatedwithanincreasing（decreasing）surfacetemperatureoverwesternNorthAmericabutadecreasing（increasing）surfacetemperatureovereasternNorthAmerica.Inwinter,centralNorthAmericawarms（cools）whentheKEfrontisstrong（weak）.Theresponseoftheatmosphericcirculation,includingwindinthehighandlowtroposphere,troughs,andridges,tothestrengthening（weakening）oftheKEfrontisthemaincauseofthesechangesinsurfacetemperature.

简介：AltynTagh差错是西藏的高原的北边界。作为在世界上的最著名的罢工滑倒差错之一，构造变丑上并且晚的大成就第四级滑倒率被造成了。然而，有AltynTagh差错是否延续到Jinta盆的长持续的争论或甚至东方。在这份报纸，我们使用卫星图象解释，领域调查，沟挖掘，和标明日期到最新在JintaNan掸人的东方结束发现NS惹人注目的陡坡的学习的光刺激的光。结果如下：第一，一组正常差错在Heihe河的平台T2上发展，全部的长度数量到40km，全部的陡坡高度是30畣慬楴杮琠敨映畡瑬猠楬獰猠潨獷氠湯?整浲愠瑣癩瑩敩?景映畡瑬?耶喩鼡?桴?慢楳?愠摮猠浯?潢湵慤祲映畡瑬?敫瑰愠瑣癩?晡整??‵吗？

简介：Eoliandustpreservedindeep-seasedimentsoftheNorthPacificOcean(NPO)isanimportantrecorderofpaleoclimaticandpaleoenvironmentalchangesintheAsianinland.Tobetterunderstandchangesinthedustprovenances,inthisstudydiffusereflectancespectroscopy(DRS)wasusedtoextracttheeoliansignalrecordedinsedimentsofODPHole885ArecoveredfromtheNPO.First,wesystematicallyinvestigatedsievingeffectsontheDRSdata;thenbandpositionsofhematite(obtainedfromthesecondorderderivativecurvesoftheK-MremissionfunctionspectrumderivedfromtheDRS)wereusedtodistinguishdifferentprovenancesoftheeoliandustpreservedinthepelagicsedimentsofthishole.Ourresultsshowthatthesieving(38μm)processcansuppresseffectivelytheexperimentalerrors.EoliansignaturesfromChineseLoessPlateau(CLP)sourcesandnon-CLP-sourceshavebeenidentifiedinthepelagicsedimentsofODPHole885AfromthelatePliocenetotheearlyPleistocene.TheprovenancedifferencesaccountforthediscrepanciesintheeolianrecordsrecoveredfromthepelagicsedimentsintheNPOandprofilesintheCLP.Temporalchangesindustprovenancesarecausedbythelatitudinalmovementofthewesterlyjetmainstream.ThehematiteDRSbandpositionisausefultooltodistinguishtheprovenanceofeoliancomponentspreservedinpelagicsediments.

简介：WhiletheAntarcticSlopeCurrent(ASC)hasbeenintensivelystudiedfortheEastAntarcticaslopeareaandtheWeddellSea,itsfateinthewesternAntarcticPeninsula(WAP)regionremainsmuchlessknown.DatafromtwocruisesconductedneartheSouthShetlandIslands(SSIs)andtheElephantIsland(EI),oneinaustralsummerof2004andoneinaustralwinterof2006,wereanalyzedtoprovideabroadpictureofthecirculationpatternoverthecontinentalslopeofthesurveyedarea,andaninsightintothedynamicalbalanceofthecirculation.Theresultsindicatethatsouthwestwardcurrentsarepresentovertheupperslopeinthestudyarea,indicatingtheASCintheWAPregion.NeartheShackletonGap(SG)northoftheEI,thesouthwestwardslopecurrentsneartheshelfbreakarecharacterizedbyawatermasscolderandfresherthantheambientwater,whichproducescross-slopedensitygradientsandthenverticalshearofthealong-slope(oralong-isobath)velocity.Theverticalshearisassociatedwithareversalofthealong-slopecurrentfromnortheastwardatsurfacetosouthwestwardindeeperlayers,oradepth-intensificationofthesouthwestwardslopecurrents.ThewatermasswithtemperatureandsalinitycharacteristicssimilartotheobservedcoldandfreshwaterisalsorevealedonthesouthernslopeoftheScotiaSea,suggestingthatthiscoldandfreshwaterisoriginatedfromtheScotiaSeaslopeandflowssouthwestwardthroughtheSG.OvertheshelfnorthoftheSSIs,thecoldandfreshwatermassisalsoobservedandoriginatesmainlyfromtheBransfieldStrait.Inthisarea,verticalstructureofthesouthwestwardslopecurrentsisassociatedwiththeonshoreintrusionoftheupperCircumpolarDeepWaterthatcreatescross-slopedensitygradients.

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简介：Theroleofwintersea-iceintheLabradorSeaasaprecursorforprecipitationanomaliesoversoutheasternNorthAmericaandWesternEuropeinthefollowingspringisinvestigated.Ingeneralterms,astheseaiceincreases,theprecipitationalsoincreases.Inmoredetail,however,analysesindicatethatboththewintersea-iceandtheseasurfacetemperature（SST）anomaliesrelatedtoincreasesinwintersea-iceintheLabradorSeacanpersistintothefollowingspring.Thesefeaturesplayaforcingroleinthespringatmosphere,whichmaybethephysicalmechanismbehindtheobservationalrelationshipbetweenthewintersea-iceandspringprecipitationanomalies.TheoceanicforcingsinspringincludeArcticsea-iceanomaliesandSSTanomaliesinthetropicalPacificandhigh-latitudeNorthAtlantic.Multi-modelCoupledModelIntercomparisonProjectPhase5andAtmosphericModelIntercomparisonProjectsimulationresultsshowthattheatmosphericcirculationresponsetothecombinationofsea-iceandSSTissimilartothatobserved,whichsuggeststhattheoceanicforcingsareindeedthephysicalreasonfortheenhancedspringprecipitation.SensitivityexperimentsconductedusinganatmosphericgeneralcirculationmodelindicatethattheincreasesinprecipitationoversoutheasternNorthAmericaaremainlyattributabletotheeffectoftheSSTanomalies,whiletheincreasesoverWesternEuropearemainlyduetothesea-iceanomalies.AlthoughmodelsimulationsrevealthattheSSTanomaliesplaytheprimaryroleintheprecipitationanomaliesoversoutheasternNorthAmerica,theobservationalstatisticalanalysesindicatethattheareaofsea-iceintheLabradorSeaseemstobetheprecursorthatbestpredictsthespringprecipitationanomaly.

简介：1.ObjectiveAseriesofMesozoic-CenozoiccontinentalsedimentarybasinsexistinNorthChina,coexistingwithcoal,oil/gas,andsaltresources.Manypreviousdrillingprojectshavebeenconductedwithinthesebasinstoexplorecoal,petroleum,andmineralresources,however,thesedatahavenotbeenintegratedduetodifferentindustriesowners.Inordertoefficientlyexplorethelarge-sized,easilyextracted,andenvironmentallyfriendly,sandstone-typeuraniumdeposits,previouscoalandoilexplorationdrilling-holedataaresystematicallycollected,processed,andanalyzedtoimprovethesandstone-typeuraniumprospectingexploitation.Atthesametime,wealsodiscussedtheuraniumsource,ore-formingprocessandmodelforthesandstone-typeuraniumdeposits.

简介：Background:Themainobjectiveofthisstudywastoexaminetheclimaticsensitivityoftheradialgrowthresponseof13easternwhitepine(PinusstrobusL.)provenancesplantedatseventestsitesthroughoutthenorthernpartofthespecies’nativedistributionineasternNorthAmerica.Methods:Thetestsites(i.e.,Wabeno,Wisconsin,USA;Manistique,Michigan,USA;PineRiver,Michigan,USA;Newaygo,Michigan,USA;TurkeyPoint,Ontario,Canada;Ganaraska,Ontario,Canada;andOrono,Maine,USA)examinedinthisstudywerepartofarange-widewhitepineprovenancetrialestablishedintheearly1960sintheeasternUnitedStatesandCanada.Principalcomponentsanalysis(PCA)wasusedtoexaminethemainmodesofvariation[first(PC1)andsecond(PC2)principalcomponentaxes]inthestandardizedradialgrowthindicesoftheprovenancesateachtestsite.TheyearscoresforPC1andPC2wereexaminedinrelationtoanarrayoftestsiteclimatevariablesusingmultipleregressionanalysistoexaminethecommonalityofgrowthresponseacrossallprovenancestotheclimateofeachtestsite.ProvenanceloadingsonPC1andPC2werecorrelatedwithgeographicparameters(i.e.,latitude,longitude,elevation)andasuiteofbiophysicalparametersassociatedwithprovenanceoriginlocation.Results:TheamountofvariationinradialgrowthexplainedbyPC1andPC2rangedfrom43.4%to89.6%.Dendroclimaticmodelsrevealedthatwhitepineradialgrowthresponsestoclimatewerecomplexanddifferedamongsites.Thekeydendroclimaticrelationshipsobservedincludedsensitivitytohightemperatureinwinterandsummer,coldtemperatureinthespringandfal(i.e.,beginningandendofthegrowingseason),summermoisturestress,potentialsensitivitytostorminduceddamageinspringandfal,andbothpositiveandnegativeeffectsofhigherwintersnowfal.Separationoftheloadingsofprovenancesonprincipalcomponentaxeswasmainlyassociatedwithtemperature-relatedbioclimaticparametersofprovenanceoriginat5ofth

简介：OnOctober18,2018,theChinaGeologicalSurveylaunchedaprojectoftheNationalKeyResearchandDevelopmentProgramofChina,entitled"PredictionandDeepExplorationDemonstrationofGoldPolymetallicDepositsintheJiaodongandLiaodongAreaswithintheNorthChinaCraton".Forthisproject,WulongandBaiyun-XiaotongjiapuyiinJiaodong,aswellasthenorthernZhaopingbeltsofLiaodong,werechosenasoreprospectingdemonstrationareas(Fig.1).

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