简介：WeiheGraben是在中国而且一个重要活跃地震地区的重要新生代差错盆不仅。Huashan山麓差错是WeiheGraben的东南方面上的一个重要活跃差错并且自从新生代，是高度活跃的。1556的著名大Huaxian县地震发生在Huashan山麓差错上。这地震，夺走约830000个人的生活，是知道发生在一个高角度的正常差错上的很少大地震之一。Huashan山麓差错是能被用来学习构造活动和联系危险的一个典型活跃正常差错。在这研究，类型和特征，沿着这个差错的近来第四级的变丑从地质的调查，历史的研究和全面分析被讨论。根据它的特征和活动，差错能被划分成三节，也就是东方、中央、西方。东方、西方的节显示正常滑倒。强烈变丑沿着二节发生了在期间第四级；然而，没有变丑发生在Holocene期间。中央节经历了重要高角度的正常差错活动在期间第四级，包括Holocene。由差错的Holocene冲积扇子和黄土切割沿着Huashan山麓差错地区的中央节在Huashan山的许多溪流山谷的嘴被识别了。Huashan山麓差错的三节，中央节是最活跃并且是很活跃的在期间晚第四级。正常蘸滑倒的率是1.67-2.71牯慧楮?慷汬摥洠捩潲潦獳汩?潣獮獩楴杮漠?楦慬敭瑮畯?祣湡扯捡整楲?愠杬污挠敯潮楢?湡?捡湡桴浯牯桰捩愠牣瑩牡档栠癡?敢湥搠'覜蠝Ｕ?牦浯渠湯'蹜T敲畯?汣祡瑳湯獥愠摮洠摵瑳湯獥漠?桴?敐灰牥?畯瑮楡獮匠慨敬?牯慭楴湯????氠'椰嫇?瑩?瑳慲潴祴数愠敲?湩琠敨倠灥数?潍湵慴湩?眠楨档愠敲瀠牡?景琠敨?汯?牃獯?潍湵慴湩?湩倠汯湡吗？

简介：BasedonanalysesoftherelationshipbetweenPacificMeridionalMode(PMM)andnumberoftropicalcyclones(TCs)activityoverthewesternNorthPacific,theimpactsofthePMMonTcactivityoverthewesternNorthPacificarestudiedusingnumericalsimulationswithanAtmosphericGeneralCirculationModel(CAM3)ofNationalCenterforAtmosphericResearch(ofUSA).TheresultshowsthatthePMMhasimpactsonthelarge-scalegeneratingenvironmentofTCs,thusaffectingtheirnumberandstrength.ThenumericalsimulationsusingtheNCARCAM3indicatethatwiththeinclusionoftheforcingfromseasurfacetemperature(SST)ofthePMM,thereappearsadecreasedmagnitudeoftheverticalzonalwindshear,largeproportionofrelativehumidity,anomalouswesterlywindatlowlevelsandanomalouseasterlywindathighlevels,inassociationwithanomalouscycloniccirculationatlowlevelsandanomalousanti-cycloniccirculationathighlevelsoverthetropicalwesternPacific.Thus,thePMMprovidesfavorableenvironmentforthetyphoongenesis.Inthesensitivityexperiment,TCshavelargerstrength,lowerSSTatthecenter,strongertangentialwindat850hPaandintensifiedwarmcoresathighlevels.Inthispaper,thesimulationresultsaresimilartothatinthedataanalyses,whichrevealstheimportantimpactofthePMMonTCactivityoverthewesternNorthPacific.

简介：在Balochistan的Kazhaba村庄附近的玄武岩的枕头熔岩在Bagh建筑群的构造裂片被发现：在穆斯林Baghophiolite建筑群下面的混合物地区。这些vol-canics被碱暗岩主要代表。岩相学和化学建议这些暴烈的岩石温和地属于到强烈碱，intra板暴烈的岩石系列。他们的低Mg#和低Cr，Ni和公司内容建议这些volcanics的父母岩浆直接没从部分融化的披风来源被导出，但是结果在一个上面的水平岩浆房间的分别，在线路到爆发。他们的LILE和HFSE，有显著积极Nb异例的充实的初发的使披风正常化的模式进一步证实他们的在内板geochemical签名并且与充实的披风来源一致。他们的高度充实的LREE模式和高度(La/Yb)N并且(Ce/Yb)N比率建议部分融化的garnet-lherzolite父母岩浆来源。Zr对Zr/Y研究建议这些volcanics从大约15%部分融化的充实的披风来源被导出。这些迟了的白垩纪intra板volcanics可以代表重聚热点的披风羽毛活动，这被建议，并且在它上在印度板的经过以前在Ceno-Tethys海洋地板的经过期间被爆发。

简介：

简介：Accordingtofieldinvestigationandinterpretationofremotesensingimages,thenorthsegmentoftheLongling-RuilifaultisaHolocenedextralstrike-slipfaultwithasmallamountofnormalfaulting.Basedonlarge-scalegeologicalmappingatsometypicallocationsandquantitativegeomorphologicdeformationmeasurementanddatinganalysis,thisfaultisaHoloceneactivefault.Thestrike-sliprateoftheLongling-Ruilifaultis2.2~2.5mm/aandverticalsliprateis0.6mm/asincethelatePleistoceneepoch.Thestrike-sliprateoftheLongling-Ruilifaultis1.8~3.0mm/aandverticalsliprateis0.5mm/asincetheHoloceneepoch.BasedonthePoissonmodel,lognormalmodelandBPTmodel,theoccurrenceprobabilityofstrongearthquakesin50yearsisestimatedtobe6.32%,0.08%and0.05%,respectively.Then,a1.82%probabilityofoccurrenceofcharacteristicearthquakeforthenorthsegmentoftheLongling-Ruilifaultisobtainedbysettingaweightof0.28,0.36and0.36tothePoissonmodel,lognormalmodelandBPTmodel,respectively.

简介：ThefaultzonealongthenorthernmarginofWestQinlingRangeisamajoractivefaultzoneinthekeyseismicmonitoringareainthesoutheasternpartofGansuProvince.Inordertostudythecurrentactivitycharacteristicsofthisfault,GPSmonitoringnetworkhasbeenarrangedalongbothsidesofthefaultand3measurementshavebeenmadefrom1996to1998.Theresultindicatesthatobviousdifferentialmovementexistsalongthenorthandsouthsidesofthefaultandtheeastwardmovementonthesouthsideis3.8mm/alargerthanthatonthenorthside.IntheGPSnetwork,theshortenedsideisgenerallyinthetrendofEWandtheextendedsideisbasicallyNWtoSE.TheprincipalcompressionalstresstrendinthisareaisaboutEWandthesinistralmotionisobviousintheeasternpartofthefault(nearWushan).Themeasuredresultsalsoindicatethatthedisplacementratehasdecreasedby50%andthecompressionalstrainhasincreasedby100%ascomparedthedataof1997～1998withthoseof1996～1997,whichshowst

简介：Onthebasisoflocatingbythegeochemicalprospecting,shallowseismicsounding,drilling,geologicalprofiling,andneogeochronologicaldating,wefirstfoundoutthedislocationamountalongtheLiaocheng-LankaoburiedfaultsincetheQuaternaryandtheageofitslatestactivityphaseanddeterminedthattheupperbreakpointbythefaultdislocationreaches20mbelowthesurface.ThelatestactivityphasewasintheearlyHoloceneandthefaultisashallow-buriedactivefault.Anaveragedislocationratealongthefaultis0.12mm/asincetheQuaternary.Thus,itisaburiedactivefaultwithintermediatetostrongmovementstrengthintheeasternChina.

简介：Thispaperintroducesthegeologicalstructurebackgroundaroundthe2014YutianM_S7.3earthquakearea,investigatesandanalyzestheregimeofsmallearthquakeactivityandthecharacteristicsofregionalseismicitypatterninXinjiangbeforetheearthquake,andcomparesthecharacteristicsoftheregionalseismicactivitywiththe2008YutianM_S7.3earthquake.Theresultsshow:12~3yearsbeforethe2014YutianM_S7.3earthquake,Xinjiangwasinaseismicactivestatewithstrongearthquakeoccurringsuccessively,andbeforethe2008M_S7.3earthquake,Xinjiangwasinthequietstateofmoderate-smallearthquakeswithM3.0~4.0.2BeforethisYutianM_S7.3earthquake,theregionalseismicactivityshowedashort-termanomalyfeature,thatis,seismicityofM≥5.0earthquakessignificantlyincreasedontheAltunseismiczoneandinthesourceareathreeyearsbeforetheM_S7.3earthquake,whileafiveyearlongquiescenceofseismicityofM≥4.0earthquakesappearedontheeastofthesourceareainarangeofabout440km.SixmonthsbeforethisM7.3earthquake,thereexistedseismicgapofM3.0~4.0earthquakesandnear-conjugateseismicbeltmagnitude3.0and4.0inthesourcearea.3ThestateofstrongearthquakeactivityandtheseismicitypatternofsmallearthquakesbeforethisYutianM_S7.3earthquakeweresignificantlydifferenttothatbeforethe2008YutianM_S7.3earthquake,andthismayberelatedtothedifferentseismogenicenvironmentsofthetwoM_S7.3earthquakes.

简介：在200-hPa之间的关系在东方亚洲沿海的水西方的太平洋(WPJS)上的西的喷气流异例，和加热的海洋的表面和摘要规模的短暂旋涡(STE)在在冬的北方太平洋上的活动异例被使用ERA-40和NCEP/NCAR分析数据检验。分析证明加热的表面和STE异例有不同模式，相应于三个WPJS异常模式分别地。在第一个WPJS异常模式，WPJS主要部分不显示出柔韧的异例。异常的西的风，经过日期线发生在中间纬度的中央东方的太平洋上与经过日期线和北方太平洋盆的中心在热带中央东方的太平洋介绍两个的异常加热被联系。同时，STE异例出现在异常的带的风的区域附近。在在第二个WPJS模式显示出的喷气力量的变化是强烈，与在自台湾东面的菲律宾海流向日本的暖流水流的加热异例有关，在喷气的区域和STE异例退出区域。第三个模式表明WPJS的northward/southward移动，它与在西方的诺思太平洋的加热异例的偶极的模式在35°N分开了的南方北方有一个统计连接。同时，STE空间排水量与在一样的方向的喷气移动一起。加热异例与大气的发行量有一个靠近的连接，并且因此改变中间纬度的baroclinicity，它然后经由内部大气的动力学增强WPJS异例，导致STE异例。

简介：Twoaspectsofanewmethod,whichcanbeusedforseismiczoning,areintroducedinthispaper.Ontheonehand,theapproachtoestimatebvalueandannualactivityrateproposedbyKijkoandSellevollneedstousetheearthquakecatalogue.Theexistingearthquakecataloguecontainsbothhistoricalandrecentinstrumentaldatasetsanditisinadequatetouseonlyonepart.Combiningthelargenumberofhistoricaleventswithrecentcompleterecordsandtakingthemagnitudeuncertaintyintoaccount,Kijko’smethodgivesthemaximumlikelihoodestimationofbvalueandannualactivityrate,whichmightbemorerealistic.Ontheotherhand,thismethodconsidersthesourcezoneboundaryuncertaintyinseismichazardanalysis,whichmeanstheearthquakeactivityrateacrossaboundaryofasourcezonechangessmoothlyinsteadofabruptlyandavoidstoolargeagradientinthecalculatedresults.

简介：在在M_W9.0地震前的不同时间空间的领域的地震活动的特征被学习。结果如下:①T他在澳大利亚的板的北方边界地区的深地震的活动是显然加强的since1994，显示出增加的频率，大小和深度，特别关于地震深度的异构的分发(也就是在500km和689km之间)。同时thes使神圣7.0显然在苏门答腊岛和它的附近是的M≥的地震也加强了，并且与一段大约1000km和宽度300km②T形成了一个加强的区域他有7.0显示出的M≥的全球强震的时间分发异常地震静止活动的特性在M_W9.0地震前并且在它的活跃句号期间的年，强震形成了在NWW方向罢工的一条地震的带。同时，有地震差距，M≥的地震形成5.0在震中和它的附近的区域。③TwoM≥的深地震7.0半年以前发生在西方并且在澳大利亚的板的北方边界地区的东方。他们之一在在哪儿的苏门答腊岛发生了，是著名的有M≥的没有深地震6.0发生在过去的三十年里。三天以前发生的中等震动的④Thespace分发展出了NWW罢工沿着澳大利亚的板的北方边界地区的地震的带。⑤T他在澳大利亚的板的北方边界地区散布的火山的活动在过去的4年里被加强了，特别在M_W9.0地震的出现前的几个月。

简介：基于每日的NCEP分析数据，OLR和卫星降雨数据，在2004的华南海夏季风(SCSSM)的活动的特征被分析。Theresults比正常和紧张比正常强壮证明SCSSM的建立很少迟了。由向西北和平的副热带的高度的地点影响了，它比正常向北方并且向西多，SCSSM在华南海区域主要是活跃的。在那里存在的明显的intraseasonal摆动和SCSSM的二个重要时期，一个人是about20-30天和另外的大约40-50天。潮湿的交通被专注于华南海和西北太平洋区域，减少向北方交通并且在南部的中国导致干旱。

简介：Inordertoevaluatetheinvolvementofthethyroidglandinreproduction,thyroidfunc-tioningwasdescribedinfemalecultivatedJapaneseeel(Anguillajaponica)inprogressivestagesofsex-ualmaturationinducedbychumsalmonpituitaryhomogenate(SPH)treatment.Serumthyroidhor-mones,thyroxine(T4)andtriiodothyronine(T3)werealsomeasuredineachstage.Thyroidglandac-tivity(epithelialcellheight)washighbeforeSPHinjection(previtellogenicstage),furtherincreasingattheearlyvitellogenicstage,thereafterdecreasingtolatevitellogenicandmigratorynucleusstages.TheprofilesofbothT3andT4changedduringvitellogenesis,beinghighduringprevitellogenicandearlyvitellogenicstages,andsubsequentlydeclining,thusmimickingthyroidglandactivity.Theseresultssuggestthatthethyroidhasrelationwitheelovariandevelopmentduringartificialmaturation.

简介：Inthispaper,accordingtotheresultsofthesatelliteimageryinterpretationandfieldinvestigation,westudytheactivefeaturesandthelatestactivetimesoftheChuxiong-Nanhuafault,theQuaternarybasinsformationmechanism,andtherelationshipbetweenthefaultandthe1680ChuxiongMs6%earthquake.SeveralQuaternaryprofilesatLvhe,NanhuarevealthatthefaulthasoffsetthelatePleistocenedepositsoftheT2andT3terracesofLongchuanriver,indicatingthatthefaultwasobviouslyactiveinlateQuaternary,TheChuxiong-NanhuafaulthasbeendominatedbydextralstrikeslipmotioninthelateQuaternary,withanaveragerateof1.6-2.Omm/a.SeveralpullapartQuaternarybasinsofChuxiong,Nanhua,andZiwuetc.havedevelopedalongthefault.The1680ChuxiongMs6%earthquakeandseveralmoderateearthquakeshaveoccurrednearthefault.TheChuxiong-Nanhuafaultaretheseismogenicstructureofthoseearthquakes,thelatestfaultmovementwasinthelate-Pleistocene,andeventheHolocene.Inlargearea,theChuxiong-NanhuafaultandtheeasternQujiangfaultandtheShipingfaultcomposedasetofNW-trendingobliqueorientationactivefaults,andthemotioncharacteristicsareallmainlydextralstrikeslip.Themotioncharacteristics,liketheredriverfaultoftheSichuan-YunnanRhombicBlocksouthwesternboundary,areconcernedwiththeescapingmovementoftheSichuan-YunnanRhombicBlock.

简介：Inthispaper,wemadeasystematicstudyonmorethan40yearsofobservationaldataoftentemporaryfault-crossingmeasurementsitesinthecapitalcircleregionofChina.Wecalculatedhorizontalandvertica1componentsoffaultslip,andhorizontalextensionorcompressioncomponents.Consideringthetectoniccharacteristicsofthecapitalcircleregionandregionalseismicity,weanalyzedthepresentfaultactivityofthecapitalcircleregionandtherelationshipwithearthquakes.Theresultsshowthecomplexityoffaultactivityintheregion:thelevelofactivityofallfaultsislow,mostfaultsareleft-lateralstrike-slipfaults;thereislessverticalactivitythanhorizontalactivityandcrustalmovementiscontrolledbyhorizontalmovement;faultactivityandearthquakeactivityhaveacertainrelationship,regionalfaultactivityincreasesbeforeanearthquake,andfaultactivityhascertainabnormalfeaturesbeforestrongearthquakes.

简介：

简介：BycomputingandclassifyingthedataofgullyoffsetobtainedfromfieldsurveysalongtheTianjingshanfaultzoneandestimatingtheagesofthreetypesofgullies,thestrike-slipratesalongthefaultzonearediscussedindifferenttimeintervalsandfaultsegments.Theresultssuggestthattheintensityofactivityalongthefaultzoneisnotstrong,butthedifferencesbetweendifferenttimeintervalsandfaultsegmentssincethelatePleistocenehavebeenobvious.Theaverageratesrangefrom0.23mm/ato1.62mm/a.Thelargestaveragerateis1.40mm/a,whichoccurredintheearlyandmiddleoflatePleistocenealongthewesternsegmentofthefaultzone.SincethelatestageofthelatePleistocene,thecenteroffaultingactivityofthefaultzonehasshiftedtothemiddlesegment,andtheaverageslipratesrangehavechangedfrom1.30mm/ato1.63mm/a.

简介：自从其22相对独立于另外的中等强壮的地震的1980，有女士5.0的26地震在Qinghai-Xizang(西藏)块的东北边缘被记录了。关于在22中等强壮的地震前的小地震活动的增加的研究显示了那项小地震活动在17中等强壮的地震前被提高。尽管增加的seismicity是在Qinghai-Xizang(西藏)块的东北边缘的普通现象，我们在由这现象预言中等强壮的地震有困难。以便通过小地震的增加的seismicity预言中等强壮的地震，这篇论文试图建议一个新方法，它通过小地震的分发模式的变化计算小地震频率基于在东北Qinghai-Xizang(西藏)块的小地震活动的特征，然后做主要应用。结果证明我们能通过新方法在中等强烈地震前在小地震的频率获得明显的异例，与这个小地震频率异例的振幅上的小空间范围效果。我们能获得对为在Qinghai-Xizang(西藏)块的东北边缘的中等强壮的地震的短期的异例索引中间。

简介：Theimpactofstrong(weak)intraseasonaloscillation(ISO)overSouthChinaSea(SCS)andSouthAsia(SA)insummerontheSCSandSAsummermonsoonandthesummerrainfallinEasternChinaarestudiedbyusingtheNCEP-NCARanalysisdataandtherainfalldataof160stationsinChinafrom1961to2010.Itisfoundthattheimpactsaresignificantlydifferentindifferentmonthsofsummer.ThestudyshowsthatinJuneandJulycyclonic(anticyclonic)atmosphericcirculationoverSCSandSAcorrespondstostrong(weak)ISOoverSCS.InAugust,however,strong(weak)ISOoverSCSstillcorrespondstocyclonic(anticyclonic)atmosphericcirculationoverSA.InJuneandAugustcyclonic(anticyclonic)atmosphericcirculationoverSouthAsiacorrespondstostrong(weak)ISOoverSAwhileastrong(weak)ISOcorrespondstoanticyclonic(cyclonic)atmosphericcirculationoverSAinJuly.Besides,inJunethestrong(weak)ISOoverSAcorrespondstocyclonic(anticyclonic)atmosphericcirculationoverSCS,whileinJulyandAugusttheatmosphericcirculationisinthesamephaseregardlessofwhethertheISOoverSAisstrongorweak.Theimpactsofthestrong(weak)ISOoverSCSontherainfallofeasternChinaaresimilarinJuneandJuly,whichfavorsless(more)rainfallinYangtze-HuaiheRiversbasinbutsufficient(deficient)rainfallinthesouthofYangtzeRiver.However,theimpactsarenotsoapparentinAugust.InSouthAsia,thestrong(weak)ISOinJulyresultsinless(more)rainfallinthesouthofYangtzeRiverbutsufficient(deficient)rainfallinYangtze-HuaiheRiversbasin.TheinfluenceontherainfallineasternChinainJuneandAugustisnotassignificantasinJuly.

简介：在从Libixia节的Jialingjiang形成的破裂的大多数静脉mineralsdeposited，Hechan区域包括大量僵绳白云石和伴随的天青石，方解石和荧石。这研究分析了性质，来源，由飞机光岩相学的液体的进化，液体包括方法，阴极射线发光图象，和稳定的同位素的作文。在白云石的二阶段的水的液体包括的homogenization温度在100和270°C之间变化。与δ18O数据，为破裂屑的降水负责的液体有δ18在10‰之间的O值并且18‰(相对降雪)。僵绳白云石和伴随的矿物质是在提高的温度的稠密的盐水的活动的结果。而且，液体从导出水兵的盐水的混合物被导出并且更深传播的分析表演流动。这液体在成岩作用期间在Sr被充实并且在骨折并且为地区性的矿化作用形成了天青石。僵绳白云石的溶解被归因于冷却Mg/Ca-decreased液体，它可以联系到一在包围碳酸盐石膏沥滤到天青石。