简介：<正>"…enableJiangxitobecometheexampleofecologicalcivilizationandpacesetterofbuildingbeautifulChina,andrealizethedreamofaprosperous,harmoniousandbeautifulJiangxithroughourearnestefforts."RecentyearshavewitnessedvigorouseffortsmadebytheProvincialForeignAffairsandOverseasChineseAffairs

简介：JiangxiDevelopmentandReformCommissionindicatedrecentlythatfiveREindustrialclusterswouldbeformedinJiangxiprovinceinthenextfewyears.After30years’

简介：Themultiple-beddedcharacteristicsofthecrustandmultiple-stagenature(geosyncline-platform-diwa)ofthetectoicevolutionarctectonicprcrequisitcsfortheformationandevolutionofthegranitoidsandthcirtungstenmineralizationinJiangxi.ControlledbythemultiPlc-stagetectonicevolution,allthegranitoidsofdiffcrcntgeo1og

简介：TheZudongandGuanxigranitesareoriginalrocksoftheionadsorption-typeHREEandLREEdepositsinweatheringcrustofgranites.TheΣREEvalueandLREE/HREEratiooftheZudonggraniteare264ppmand0.81-0.24respectively,andtheaverageY/ΣREEratiois35.8-54.5%.Thisismainlyduetomagmaticcrystallizationandevolutionanddeutericmetasomatism(albitization,muscovitizationandfluorite-doveritization).Thesealterationsresultedinendogenicmineralizationsofyttrium-groupREEfluorinecarbonates,silicatesandarsenates.TheGuanxigraniteischaracterizedbyLREEenrichment(theaverageLREE/HREEratiois2.43).

简介：SituatedinthenortheasternpartofJjangxiProvince,southChina,Jinshangolddepositgcotectoni-callybelongstoapartoftheDekingmini-crustobody.A8asub-elementofthesoutheasternsectionofJjangnancrustobody,theDekingmini-crustobodyislimitedtothenorthwestbyZhanggongshanmini-crustobodywiththeboundaryofLc’anjtangfaul

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简介：JiangxiZhengbangGroupCompany,Ltd.willconstructa200kt/aaceticacidunitinYima,Henanprovince.Thisunitwilladopttheadvancedmethanoloxo-synthesistechnologybasedonmethanolandcarbonmonoxideasthefeedstocksfeaturinglowinvestment,lowcost,lowenergyconsumptionandlowcontamination.Yimacityhasabundantcoalresources,andthecapacityofexistingmethanolunitsandmethanolunitsunderconstructionwillreach540kt/a.

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简介：<正>O.IntroductionGoldiscommonlyconsideredaninertelement,butitsgeochemicalpropertiesarenotsoinert.Intheareaofgolddepositstheconecntra-tionsofgoldinwaterarehigh.Itcannotonlymigrateinwater,butalsoeasilyprecipitateifthechemicalconditionschange.Thisisimpor-tantbothinprospectingforgoldbyhydrogeochemicalmethods,andingoldformation.

简介：一张新oviraptorid恐龙Jiangxisaurusganzhouensis情报。etsp。nov，从Ganzhou城市的上面的白垩纪Nanxiong形成基于一架部分骨骼被树立，江西省。新taxon不同于另外的oviraptorids在弱更低的颚的downturned坛，有在附近是的height-to-length比率的伸长大部分的上颚20%并且到大约0.70的肱骨的半径的长度比率。这种不仅把一个新成员加到oviraptorid恐龙，而且在南部的中国关于oviraptoridpaleogeographical分发提供更多的信息。

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简介：Inrecentyears,moreandmoreconflictshaveemergedinthemanagementofnaturereserves,ofwhichthemainproblemisthathowtocarryoutthecampaignofconservationalongwiththepromotionofdevelopmentoflocaleconomics.ToresolvetheactualprobleminNanjishanNationalWetlandNatureReserveandexploretheidiographicmethodofthemanagementofthewetlandreserve,somestudyingmethodsincludingface-to-faceinterviews,informaldiscussionwithlocalleadersandofficials,groupdiscussionwithlocalfishers,questionnaire,andjoboftheconversationstationhavebeencarriedout.Theresultsshowthattheeducationlevelofthelocalpeopleislow;only5%ofthelocalpeoplehaveanopportunitytothejuniorcollege;themainincomeofthelocalpeopleisfishing,whichaccountsfor70%moreorless;andtheincomeiscomingdownyearbyyearbecauseoftheunreasonablewayoffishing.Tocopewiththeproblems,somereformativewayofmanagementandthedevelopmentofthereserveareintroduced,suchasestablishinganNOGthatconstitutesoflocalfishermentoachievethegoalofcommunityco-management,developingBedandBreakfastandsoon.Throughpracticeofthemanagementoftheparticipationofthelocalpeople,wedrawtheconclusionthatthelocalpeoplehaveagreatdesiretoimprovetheirlifelevel,andtomaketheco-managementofthereserveeasy,itisimportantforthemanagerstoplaytheroleofpilotincludingengraftingthenewideas,givingsomesubsidytoencouragethelocalpeopletotakepartinthemanagement.Inaddition,makinglocalpeopleperceivevalueofthereserveandthecloserelationbetweenreserveconservationandthepromotionofleveloftheirlife.Onthisbasis,theyinclinetotakepartinthemanagementofthereserve.

简介：福雷斯特植被碳模式为评估碳排放和累积是重要的。许多方法被用来然而，在以前的研究模仿森林植被碳存货的模式无常显然在不同方法的结果之间存在，甚至在不同研究的一样的方法的估计。三个以前的方法，包括空气植被相互作用模型2(AVIM2)，Kriging，卫星数据基于的途径(SBA)，和一个新方法，当模特儿的高精确性表面(HASM)，被用来在中国在江西省模仿森林植被碳股票模式。交叉验证被用来评估方法。省的规模上的四个方法的无常和适用性被分析并且讨论。结果分别地证明HASM有最高的精确性，它在50.66%，33.37%和28.58%改善了，与AVIM2，Kriging和SBA相比。森林生物资源碳存货的模拟的无常主要从为错误，采样错误和森林区域的统计错误建模被导出。全部的森林碳存货，碳密度和江西的森林区域是288.62Tg，3.06kg/m2和94.32湡穩瑡潩n

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简介：TheYongpingcoppcrdepositissituatedinYansbanCounty,JjangxiProviencc,SouthChina.It’sacopper,sulphur,tungstenandmolybdenumpolymetallicdeposit,andhostedbytheCarboniferousvolcanicsedAnentaryrocksinwhicbYanshaniangraniticporphyries(l35-l6lMa)intruded.Ourstud-jesrevealthemajorconstrainingfactoronmetallogen

简介：ThePengshanSn-Pb-ZnpolymetallicorefieldislocatedintheJiujiang-Ruichangregion,whichisasegmentofthemiddle-lowerYangtzeRivermetallogenicbelt.ThePengshanlateYanshanianburiedplutonwithgraniticcompositionisacalc-alkalinepluton,intrusionofwhichisresponsiblefortheformationoftheSn-Pb-Znpolymetallicdepositthroughprovidingthermodynamicconditionandore-formingmaterial.Thelong-activebasementriftsinitiallyformedintheJinningperiodandthedomalstructurewithinducedsecondaryorderfaultsformedbyemplacementofthepluton,suchasring-detachmentfault,top-detachmentfaultandjointfissure,actasthepassage-wayformagmaandore-formingfluidandimpoundingstructurefororedeposit.ThemagmatoformtheplutonwithDI＞90isintensivelydifferentiated.Thevariationoftheore-formingfluidincompositionwithfallingintemperaturecausedbyactionofmagmatichydrothermalconvectionsystemcombinedwithgroundwaterconvectionsystemattributestomineralizationofvarioustypesintheorefield.Themineralizationprocesscanbedividedintosixstages,i.e.,greisenization,skarnizationofearlystage,fluorite-stanniferoussilicationstage,skarnizationofadvancedstage,quartzandcassiterite-sulfurationstageandcarbonationstage.Themineralassemblagesformedindifferentmineralizationstagesaredifferentowingtotemperaturechangingandmaybeoverlappedinspace.Malayaiteisrecognizedfromthemineralassemblageformedinthefluorite-stanniferoussilicationstage.TheoresinthePengshanSn-Pb-ZnpolymetallicdepositarespatiallyzonedwithvariationfromAs-SnmineralassemblageofhightemperatureintheinnerzonethroughSn-PbandPb-Zn-Agmineralassemblageofmiddletemperatureinthemiddlezonetofluoritemineralassemblageoflowtemperatureintheouterzone.TheexchangingofSn,MgandFebetweenbiotiteandhydrothermalfluidresultedfromvariationofphysicochemicalconditionduringevolutionprocessesofthehydrothermalflu

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简介：ReportedinthispaperaretheNdisotopiccompositionsofthepre-SinianandSinian-CambriansedimentaryrocksintheXiushuiarea,JiangxiProvince.SignificantdifferencesarenoticedbetweenthemintheirNdisotopicdompositions.Asforthepre-Sinianlightlymetmorphozedsedimentaryrocks,^143Nd/^144Nd=0.512000-0.512214,CNd(T)=-8.04-9.99,andTDM=18332426MaaresuggestedfortheSinian-Cambriansedimentaryrocks.ThesedifferenceswouldreflectthediversityofmaterialsourceforthesedimentaryrocksdepositedbeforeandaftertheSinianperiod.Mantlematerialap-pearstohavebeeninvolvedintheformationofthepre-Siniansedimentaryrockswhilethepost-Siniansedimentaryrocksarecomposedmainlyofrecycleddetritusfromthecontinentalcrust.