简介:<正>REPLACEMENTPATTERNSOFGEOTECTONICUNITSLiYuping(Dept.ofChemicalScienceandEngineering,HunanUniv.,Changsha,China,410082)replacementpattern,geotectonicunit,DiwatheoryBaseupontheDiwatheoryandthestudiesofevolutionprocessofgeotectonicunits,thispaperhasadvancedthattherearemanyreplacementpatternsofthegeotectonicu-nitsintheirevolutionprocess.Therearethreereplacementpatterns(eg.suddenchange(nor-mal)pattern,gradualchangeandprogressivepattern)duringtheplatformregionsubstitutesthegeosynclinalregionandthreereplacementpatterns(eg.normalpattern,surpassivepatternandprogressivepattern)whentheDiwaregiondevelopsfrompre-Diwaregions.Theknowl-edgeoftheseregularityisofimportantsignificanceforustodeeplystudytheevolutionofgeo-tectonicunitandthedevelopmentofthecrust.
简介:ThenorthernmarginoftheAlxablockisthejunctionofatectonicunits.Fourfirst-ordertectonicunitsaredistinguished:1.theYaganstructuralzonecharacteristicofanimmatureislandarc;2.theZhusileng-Hangwulastructuralzone,whichwasapassivecontinentalmarginintheEarlyPalaeozoicandwastransformedintoanactivecontinentalmarginintheLatePalaeozoic;3.theShalazhastructuralzonecharacteristicofamatureislandarc;4.theNuru-Langshanstructuralzone,whichwasaProterozoicorogenicbeltandlaterevolvedintoanextensionaltranstionalcrustinthePalaeozoic.Theabove-mentionedtectonicunitsdifferremarkablyinsedimentaryformations,magmaticrockassociations,metamorphismandgeochemistryandareboundedbyfaultsbetweenoneanother.
简介:杰克起来,单位广泛地在在全世界钻工程正在起一个成功的作用,并且他们的安全和效率在研究和工程实践拿越来越多的吸引力。spudcan穿入深度的精确预言在决定杰克起来联合起来是否是可行的在这个地点操作是相当有帮助的。太大的穿入深度的预言可以在随后的抽取过程由于潜在的困难导致犹豫或甚至一个地点的拒绝;一样在操作期间由于可能的不稳定性的问题太小的深度预言是真的。然而,在预兆的结果之间的偏差和最后的地数据通常存在,特别当strong-over-soft土壤在阶层被包括时。最终的决定在很大程度上有时取决于实际经验,不是指南给的预兆的结果。它是有点危险的,但是没有选择。因此,特别在有strong-over-soft土壤侧面的阶层,为spudcan穿入深度的一个可行预兆的方法着急地被需要由杰克起来工业。鉴于这,预言spudcan穿入的方法上的全面调查被执行。为不同土壤侧面的类型,为spudcan穿入深度的预兆的方法被建议,并且相应实验也被进行验证这些方法。另外,验证建议方法的可行性推进,在华南海遇到的一个实际工程盒子是也介绍了,并且相应数字、试验性的结果也被介绍并且讨论。
简介:在2010Yushu地震以后的二个小时,摇晃的紧张分发用基于地点效果的ShakeMap快速的产生系统被获得,由作者发展了,它集成原因的差错的构造设置,罢工和规模的信息,在西方的中国的焦点的机制solutions.fault破裂进程和变细关系,以及本地地点effects.The结果如下:摇紧张分发的主要的轴被指导NW-SE,平行到Yushu差错;meizoseismal区域到达紧张并且盖住300km2;紧张区域主要沿着原因的差错在区域40km东南和震中的15km西北被散布;由于本地土壤条件,有基岩上的紧张的区域的西北的部分看紧张是否从基岩变换成土壤;有紧张的区域,,分别地测量3,000km2,8,000km2,和24,000km2。
简介:OnApril14,2010at07:49(Beijingtime),acatastrophicearthquakewithMS7.1occurredatthecentralQinghai-TibetanPlateau.TheepicenterwaslocatedatYushucounty,QinghaiProvince,China.Atotalof2036landslidesweredeterminedfromvisualinterpretationofaerialphotographsandhighresolutionremotesensingimages,andverifiedbyselectedfieldinvestigations.Theselandslidescoveredatotalareaofabout1.194km2.Characteristicsandfailuremechanismsoftheselandslidesarelistedinthispaper,includingthefactthatthespatialdistributionoftheselandslidesiscontrolledbyco-seismicmainsurfacefaultruptures.Mostofthelandslidesweresmallscale,causingratherlesshazards,andoftenoccurringclosetoeachother.Thelandslideswereofvarioustypes,includingmainlydisruptedlandslidesandrockfallsinshallowsandalsodeep-seatedlandslides,liquefactioninducedlandslides,andcompoundlandslides.Inadditiontostronggroundshaking,whichisthedirectlandslidetriggeringfactor,geological,topographical,andhumanactivityalsohaveimpactontheoccurrenceofearthquaketriggeredlandslides.Inthispaper,fivetypesoffailuremechanismsrelatedtothelandslidesarepresented,namely,theexcavatedtoesofslopesaccompaniedbystronggroundshaking;surfacewaterinfiltrationaccompaniedbystronggroundshaking;co-seismicfaultslippingaccompaniedbystronggroundshaking;onlystronggroundshaking;anddelayedoccurrenceoflandslidesduetosnowmeltorrainfallinfiltrationatsiteswhereslopeswereweakenedbyco-seismicgroundshaking.Besidesthemainco-seismicsurfaceruptures,slopefissureswerealsodelineatedfromvisualinterpretationofaerialphotographsinhighresolution.Atotalof4814slopefissures,withatotallengthupto77.1km,werefinallymapped.Theseslopefissuresaremainlydistributedontheslopeslocatedatthesoutheasternendofthemainco-seismicsurfacerupturezone,anareasubjecttostrongcompressionduringtheeart
简介:1988年,Ongkiehong等在其“关于通用地震数据采集技术”一文中陈述了采用96道地震仪陆上作业是通过减少线性组合,增加最大偏移距,走向不均匀采样的第一步。通用采集意指我们在采集期间不再被迫提交处理或者最终解释网格,但是在后来的各个时期,我们有改变处理、解释面元大小的能力,它取决于在研究中对特殊处理、解释目标的采样需要。Ongkiehong等(1988年)称之为“不受约束的采集”。2000年在沙特阿拉伯,我们动用了一个高密度、单扫描的2880道地震队,配备有每道单检波器串,每串12个检波器,完成了通用陆上采集任务。对于二维中间放炮排列采集而言,这种观测形式准许记录7200m偏移距、纵向采样间隔为非常密集的5m地震数据。满覆盖采集(即炮点距为5m)产生了2+5m的共中心点(CMP)距、正常1440次覆盖的数据采集。这种密集的空间采样间隔并结合重叠排列,保证了整个波场在期望的空间频带宽度内无假频,并且对所有目的层(浅、中、深层)均可满足二雏覆盖要求。因为非常复杂的近地表盖层覆盖了深部含油气目的层,所以这一点是非常有意义的。因此,勘探目标激励计算中心具有处理5米间距原始数据的选择方案。它用一个受限制的全偏移距和时间变化范围解决近地表问题并用叠加或以上所论述的5m倍数(如25或30m)的任一采样间距产生野外记录。实际上,从常规480道二维地震队转变为通用单扫/单串2880道地震队的采集成本相近,这是因为野外工作量相同(每线性千米的扫描数和检波器串数)。这种通用采集的转变需要约定、对策而且是综合考虑的。本文选了3个高密度野外采集试验,论证了高信噪比区的资料品质,重新分析不受约束的野外排列设计的综合影响和提高较差资料区的信噪比的处理,同时检验
简介:Acomprehensivestrengthmonitoringsystemusedonafixedjacketplatformispresentedinthispaper.Thelong-termmonitoringofW-11-4Aplatformachieved.Structuralresponses(strainandacceleration)atselectedlocations,aswellasassociatedenvironmentalparameters,havebeenobtained.Theemphasisofthepaperisplacedonthesystemdesign,andtheinstrumentationandoperationmethodologyemployedinthemonitoringofthestructuralresponses.Theperformanceofthesystemandthecharacteristicresultsobtainedduringits13-monthoperationarealsosummarized.
简介:AnearthquakewithM7.1occurredinYushu,QinghaiProvince,China,at07:49a.m.onApril14,2010,accordingtotheChineseSeismicStationNetwork.Thesequenceisafore-mainafter-shocktypesequence.AforeshockwithM4.7occurred2hoursand11minutesbeforethemainshock.Therewere12foreshocksand2385aftershocksuntilJune31,2010.Inwhich,thereare21aftershocksbetweenM3.0andM3.