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简介：<正>AttheinvitationoftheChineseAssociationforInternationalUnderstanding(CAFIU),a10-memberNGOdelegationcomposedofrepresentativesfrommedia,thinktanksandNGOsfromBangladesh,IndiaandSriLankavisitedChinafromApril9to18.Ontheseconddayofarrival,thedelegationvisitedXichengDistrictAdministrativeServiceCenter.Thecenterprovidessuchservicesas

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简介：Wanan盆的延期和沉淀上的量的研究被执行基于可得到地震并且和地区性的地质的数据的地上凿穿数据。用平衡剖面图和backstripping技术，我们重建了stratigraphic免职和盆的构造进化历史。形成从的盆始新世并且除了晚中新世的本地人通常处于一个extensional/transtensional国家compressoin。在渐新世并且早的主要的盆延期ocurred中新世(在∼16.3妈前)并且处于更小的率的此后一致的段。北、中间的盆在38.6-23.3妈期间更早强烈地延长了，当南部的盆主要在23.3-16.3妈期间被拉长时。盆形成和发展与轮流出现有关对沿着Wanan差错地区的右罢工滑倒运动左首。主导的动力学可以被华南海传播的seafloor引起并且它的外部板相互作用。盆构造进化被划分成五个阶段：起始的rifting，主要rifting，裂缝飘移转变，结构的倒置，和热沉淀。

简介：Integratedstudiesofverticalsedimentarysequences,grainsizes,andbenthicforaminiferaandostracoda,incombinationwithAMS14Cdating,and210Pband137CsanalysiswerecarriedoutinthreevibracorestakenfromtheareaofrelictdepositsonthewesternSouthYellowSea.Therelictsands,whichareabout0.4mthick,overlieontheEarlyHolocenecoastalmarshortidalflatdepositswithanevidenterosionalinterfaceinbetween.Themiddleandupperpartsorsometimesthewholeoftherelictsandshavebeenreworkedunderthemoderndynamicenvironment.Thesedimentationratevariesbetween0.20–0.30cmyear-1.Therelictsandsshowabimodalgrain-sizedistributionpatterninfrequencycurves,withasharppeakinthecoarsefractionbetween3Φand4Φandasecondarypeakinthefinefractionofabout7Φ.Ofthebenthicforaminiferalandostracodassemblages,thereworkedrelictsandsarecharacterizedbythemixingofthenearshoreeuryhalineshallow-waterspeciesanddeeperwaterspecies.TheerosionalinterfaceatthebottomoftherelictsandsisconsideredasaregionalravinementsurfaceformedduringthetransgressionintheEarlyHoloceneduetoshorefaceretreatinglandwards.Therelictsandswereaccumulatedontheravinementsurfaceduringthetransgressioninthedeglaciationperiodaslagdepositsafterwinnowingandreworkingbymarinedynamicprocesses.Andthesecondarypeakoffinefractioninthefrequencycurvefortherelictsandssuggeststheinputoffine-grainedsedimentsduringthereworkingprocess.Astheconclusion,therelictsandsinthestudyareaareinterpretedasatypeofreworkedrelictsediments.

简介：由于山论的阻塞，弱风醒来在华南海发生在夏天离开东北越南。在风下面醒来，温暖的水从两个高分辨率的卫星数据和水道学的观察被观察。温暖的水的wake在6月形成，继续在7月和8月成熟，开始在9月腐烂，并且消失在10月。温暖的水也弄醒表演柔韧日报它在日子期间加强并且在夜里变弱的变化。温暖的水醒来能通过导致风的混合被产生并且热(潜伏的热流动)过程。在这份报纸，一个混合的层模型被用来分别地在季节、日报的timescales上评估二个过程的相对重要性。结果比导致风的混合在季节的timescale上处理的证明热过程做更大的贡献到wake，当时温暖的水醒来被导致风的混合统治过程在上一日报timescale。

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：根据为系统(ROMS)建模的地区性的海洋，在华南海(SCS)的thermocline的季节的变化数字地被调查。模仿的水动力学根据以前的研究：在SCS的发行量模式在冬季是气旋的并且在夏天，和如此的一个变化逆旋风被季风风主要驾驶。在巡航获得的建模的温度侧面和观察之间的错误在海洋的上面的层是相当小的，显示海洋地位相当被模仿。根据垂直温度侧面的形状，五种thermocline类型(浅thermocline，深thermocline，混合thermocline，两倍thermocline，和多重thermocline)此处被定义。在冬季，什么时候在东北，季风占优势，在SCS的西北的很浅的架海很好被混合，并且没有明显的thermocline。深区域通常有深thermocline，并且混合或双的thermocline经常在SCS的南方在冷旋涡附近发生在区域。在夏天，当西南的季风占优势时，有浅thermocline的架海区域极大地膨胀。不同thermocline类型的分发与海洋深测术显示出一种关系：从对深水浅，thermocline类型通常变化从对浅或混合深，thermocline，和双或多重的thermocline通常发生在陡峭的区域。三个主要thermocline特征(上面的界限深度，厚度，和紧张)的季节的变化也被讨论。因为SCS也是热带气旋经常发生的一个区域，到在短时间规模的一个台风过程的thermocline的反应也被分析。

简介：为了加强国内外心脑血管专业高新科技信息交流，提高老年医学领域的基础研究与临床治疗水平，促进年轻医务工作者专业技能的快速成长与发展，《中华老年心脑血管病杂志》作为学术前沿的交流平台，于2013年12月5日与位于美国旧金山硅谷的CaliforniaSouthBayUniversity（CSBU）即美国加州南湾大学商定，双方坦诚牵手开展长期协作。

简介：ThispaperstudiesthecurrentavailableoptionsforfloatingproductionplatformsindevelopingdeepwateroilfieldsandthepotentialdevelopmentmodelsoffutureoilandgasexplorationintheSouthChinaSea.Adetailedreviewofcurrentdeepwaterplatformsworldwidewasperformedthroughtheexamplesofindustryprojects,andtheprosandconsofeachplatformarediscussed.Fourtypesofplatformsarecurrentlyusedforthedeepwaterdevelopment：tensionlegplatform,Spar,semi-submersibleplatform,andthefloatingproductionsystemoffloading.Amongthese,theTLPandSparcanbeusedfordrytreeapplications,andhavegainedpopularityinrecentyears.Thedrytreeapplicationenablestheextensionofthedrillingapplicationforfixedplatformsintofloatingsystems,andgreatlyreducesthecostandcomplexityofthesubseaoperation.Newlybuiltwettreesemi-submersibleproductionplatformsforultradeepwaterarealsogettingtheirapplication,mainlyduetothemuchneededpayloadfordeepwatermakingtheconversionoftheolddrillingsemi-submersibleplatformsimpossible.Theseplatformshavebeenusedindifferentfieldsaroundtheworldfordifferentenvironments;eachhasitsownadvantagesanddisadvantages.Therearemanychallengeswiththesuccessfuluseofthesefloatingplatforms.Alotoflessonshavebeenlearnedandextensiveexperienceaccumulatedthroughthemanyprojectapplications.Keytechnologiesarebeingreviewedforthesuccessfuluseoffloatingplatformsforfielddevelopment,andpotentialfuturedevelopmentneedsarebeingdiscussed.SomeofthetechnologiesandexperienceofplatformapplicationscanbewellusedforthedevelopmentoftheSouthChinaSeaoilandgasfield.

简介：ToinvestigatetheannualandinterannualvariabilityofoceansurfacewindovertheSouthChinaSea(SCS),thevectorempiricalorthogonalfunction(VEOF)methodandtheHilbert-Huangtransform(HHT)methodwereemployedtoanalyzeasetofcombinedsatellitescatterometerwinddataduringtheperiodfromDecember1992toOctober2009.ThemergedwinddataweregeneratedfromEuropeanRemoteSensingSatellite(ERS)-1/2Scatterometer,NASAScatterometer(NSCAT)andNASA'sQuickScatterometer(QuikSCAT)windproducts.ThefirstVEOFmodecorrespondstoawinter-summermodewhichaccountsfor87.3%ofthetotalvarianceandrepresentstheEastAsianmonsoonfeatures.ThesecondmodeofVEOFcorrespondstoaspring-autumnoscillationwhichaccountsfor8.3%ofthetotalvariance.Toanalyzetheinterannualvariability,theannualsignalwasremovedfromthewinddatasetandtheVEOFsoftheresidualswerecalculated.ThetemporalmodeofthefirstinterannualVEOFiscorrelatedwiththeSouthernOscillationIndex(SOI)withafour-monthlag.ThesecondtemporalinterannualVEOFmodeiscorrelatedwiththeSOIwithnotimelag.ThetimeseriesofthetwointerannualVEOFsweredecomposedusingtheHHTmethodandtheresultsalsoshowacorrelationbetweentheinterannualvariabilityandElNi?o-SouthernOscillation(ENSO)events.

简介：TheresponseoftheSouthChinaSea(SCS)toTyphoonChanchu(2006)wasexaminedusingtheMM5andPOMmodel.InthePOMmodel,seasurfaceboundaryconditionswereforcedbythesimulationwindfieldfromMM5,thevelocityforcingwasintroducedintheeasternboundaryandthecomputationalschemesofheatfluxesatthesurfacewereintroduced.Comparisonwiththeobservationdatashowsthatthesimulatedresultsarereliable.IntheresponseprocessoftheSCStoTyphoonChanchu,theinfluenceoftheheatfluxesonthermalstructureoftheSCSwasregionallydifferent.Strongwindforcingwouldleadtoupwellingphenomenoninthelateralboundaryofdeepwaterbasin.Furthermore,theEkmanpumpingtheorywasusedtodiscusssubsurfaceupwellinganddownwellingphenomenonintyphoonforcedstage.

简介：源自陆地的siliciclastic的一个序列在Baxiandun外面摇庄稼，Qingdao，在在诺思中国之间的中生代collisional边界附近，块(网络控制块)和华南堵住(SCB)。这些低档变形了siliciclastic岩石被greywacke与页岩统治，manganiferous有细密纹理的沙岩，arkose和集团企业层。关于这些岩石的形成有二基本解释。一个人认为这个序列在网络控制块以内被形成，并且是白垩纪Laiyang组和Qingshan组的部分河的外形和暴烈的碎片外形出现在山东地区性的地质的地图上。另一条意见建议这些岩石表示在斜坡和盆外形的混浊depositional系统主要在奥陶纪被扔。重要地基于地观察，petrological分析，和大多数，在这的geochemical结果学习，在Baxiandun节的沉积阶层主要由siltstone，沙岩和mudstone岩性学组成。他们被深海的碎片和混浊存款在一个湖的斜坡和底统治。在Baxiandun节岩石标明日期的U-Pb由岩屑形成的锆石显示来源岩石是很复杂的，他们的年龄被改变从对早白垩纪太古代。源自陆地的岩屑的最年轻的年龄能代表沉积阶层的年龄。因此，我们推断沉积岩石属于早白垩纪深海的湖的沉积序列并且从SuluUHPorogen和华南块边缘的侵蚀有多重来源origined。

简介：最早三叠纪的Yinkeng形成在著名Meishan节被暴露，华南，它为二叠三叠纪的边界(PTB)包含节和点(GSSP)的全球Stratotype。它记录有韵律的引申主要由marlstone和石灰石包括了的厘米规模。在捆的五种类型嵌入的两行诗的七种类型基于lithologic单位的出现和厚度被认出，建议他们的形成被周期的过程控制。观察的周期的各种各样的订单相关很好，另外的早三叠纪的对应物在华南记录了。这里，我们现在的新cyclostratigraphic基于lithologic厚度和Yinkeng形成的相对碳酸盐内容结果。碳酸盐内容的力量系列证明在整个形成认出的主要波长的比率类似于100kyr的短怪癖，33kyr斜，和21kyr领前周期，显示天体的信号在最早三叠纪的有韵律的继任被记录。在从费歇尔阴谋获得的显著lithologicrhythmicity和海平面的变化之间的坚固性显示高周波的气候的周期可能在PTB集体扑灭以后立即驾驶了海平面的变化。而且，从沉积记录解释的海平面的变化与100kyr匹配很好的4th顺序碳酸盐内容的短怪癖部件，思考短导致怪癖的气候改变的100kyr可能多半控制了4th顺序序列的免职，这从有韵律的继任认出了。

简介：南方Qinling的构造进化，是Qinlingorogenic带的主要部分，仍然在争论和南方Qinling的变丑历史糟糕被学习。在这份报纸，详细说明了结构，微结构，石英c轴织物分析，和在南方Qinling的Madao片麻岩的地球年代学结果被介绍描绘变丑历史。结果证明在北部分(Tiefodian-Laozhanggou)的岩石经历一般的砍并且在相对低温度使变形。shear感觉通常是到北方的南方。相反，在南部的部分(Laozhanggou-Panjiahe)的岩石微弱地被砍与纯砍高温度的变丑的特征和证据。基于分析，我们在那里结束那存在我们能划分的在Madao片麻岩并且因此的二不同变丑几何学变丑进二个阶段。早阶段被地区性的弄短代表，当迟了的阶段特征向北方推进了砍时，证据证明它是在他们之间的一个进步过程。从pre-deformationalmigmatite静脉锆石与约会的LA-ICP乌普布女士产出198.5±的年龄2.0妈。在有post-deformational花岗石的年龄的联合，这结果显示向北方，戳Madao片麻岩砍发生了在晚三叠纪。鉴于在南方Qinling的这些结果和另外的报导数据，我们建议在Madao片麻岩的那变丑可以源于起始的碰撞并且随后向北方生长在晚三叠纪。

简介：ThisstudyexaminesthemodulationoftropicalcyclogenesisovertheSouthChinaSea(SCS)bytheElNio-SouthernOscillation(ENSO)Modokiduringtheborealsummer.Resultsrevealthatthereweremoretropicalcyclones(TCs)formedovertheSCSduringcentralPacificwarmingyearsandlessTCfrequencyduringcentralPacificcoolingyears.Howdifferentenvironmentalfactors(includinglow-levelrelativevorticity,mid-levelrelativehumidity,verticalwindshear,andpotentialintensity)contributetothisinfluenceisinvestigated,usingagenesispotential(GP)indexdevelopedbyEmanuelandNolan.CompositeanomaliesoftheGPindexareproducedforcentralPacificwarmingandcoolingyearsseparately,whichcouldaccountforthechangesofTCfrequencyovertheSCSindifferentENSOModokiphases.Thedegreeofcontributionbyeachfactorisdeterminedquantitativelybyproducingcompositesofmodifiedindicesinwhichonlyoneofthecontributingfactorsvaries,withtheotherssettoclimatology.Theresultssuggestthattheverticalwindshearandlow-levelrelativevorticity,whichareassociatedwiththeENSOModoki-inducedanomalouscirculationsinMatsuno-Gillpatterns,makethelargestcontributionstotheENSOModokimodulationoftropicalcyclogenesisovertheSCSasimpliedbytheGPindex.TheseresultshighlighttheimportantrolesofdynamicfactorsinthemodulationofTCfrequencyovertheSCSbytheENSOModokiduringtheborealsummer.

简介：CertaineffectshavebeenachievedintheChina-SouthAsiapeople-to-peoplediplomacy,demonstratedbyincreasinglyactiveevents,betterenvironmentfordevelopment,abigleapineconomicandtradecooperation,furtheropeningupofthepeople-to-peopleandculturalexchangesandgrowingimportanceoftheacademicandthink-tankdialogues.Still,inadequaciesofpeople-to-peoplediplomacytowardsSouthAsiaremain,manifestedbyunbalancedexchangepatternandratherweaksocialinfluenceawaitsfurtherenhancement.Inordertomakeuptheinadequacies,theauthorscontendthatthefollowingmeasuresneedtobeadopted:1)tofullyplaythegovernment’sroleandbreaktheexistingbottleneckinpeople-to-peoplediplomacy;2)tolistmediaexchangeandstudy-abroadprogramaskeyareasoftheagenda;3)togiveatrialofconductingpeople-to-peoplediplomacyincasesofBhutanandMaldives,exploringcomparativeadvantagestoofficialdiplomacy.Theseproposalsmayvary,however,theaimtoexpandtheoptimalreachofChina-SouthAsiapeople-to-peoplediplomacywithcreativeforms,leavesunchanged.InChina’soveralldiplomaticagenda,SouthAsiaownsquadri-categories,whicharemajorpowers,neighboringanddevelopingcountriesandmultilateralregions.Undoubtedly,SouthAsiaisentitledtostatusandimportancebecauseofthesecharacteristics,covering8sovereigntycountriesofgreatdifferences,namelyIndia,Pakistan,NepalandMaldivesetc.Throughouthistory,ChinaandSouthAsiahavewitnessedlong-standingculturalexchanges,gradualdeepeningofeconomicandsocialcontacts,closerintimacyamongpeoples’interactionsandprosperousdevelopmentofpublicdiplomacy.Despiteofallthese,problemsremainunsolvedthatneedfurtherconsiderationandsolutioninresponse.

简介：自动化鉴定并且mesoscale海洋旋涡追踪最近在物理海洋学成为了一个研究热点。几个方法被开发了并且适用在华南海(SCS)调查海洋旋涡的一般运动、几何的特征。然而，很少的研究试图检验内部进化处理的旋涡。在这研究，我们报导了一个混合方法基于他们的内部结构在SCS跟踪旋涡繁殖，它被旋涡中心，脚印边阶，和合成边阶描绘。埃迪鉴定和追踪的结果被一个官方补给底的空间与时间的模型代表。消失，再现，裂口，和合并的立刻的国家，动态进化过程，和事件的信息在一个GIS数据库被存储。结果被在北SCS对十个Dongsha气旋的旋涡(数据通信设备)和三个长寿逆旋风的旋涡(王牌)比较验证，它在以前的文学被报导。我们的学习证实了这些旋涡的发展。而且，我们在我们的数据库从2005～2012在这些区域发现了更像数据通信设备、像王牌的旋涡。消失，重现，切开，并且合并活动的空间分发分析证明在SCS的旋涡趋于到簇到吕宋岛岛的西北，吕宋岛海峡的西南，并且在越南的边缘的海附近。在这些区域的自台湾东面的菲律宾海流向日本的暖流侵入和复杂的海地板地形学是导致这些空间簇的可能的因素。