简介:OnApril25,2015,aM_S8.1earthquakeoccurredinNepal.IntheTibetareaofChina,thisearthquakecausedheavycasualtiesanddamagetohousing,roads,communications,otherlifelineengineering,waterconservancyandotherinfrastructure.Thispaperintroducesthebasicsituationoftheearthquake,andbasedontheinvestigationandassessmentofseismicintensity,thedamageofthedisasterareaisanalyzed,andbuildingtypesanddamagetothelifelinesystemsandvariousindustriesaregiven.Throughtheanalysisofthecharacteristicsoftheearthquakedisaster,thispaperpointsouttheexistingproblemsinseismicfortification,andfinallyputsforwardproposalsforthepreventionandcontrolofearthquakegeologicaldisasters,scientificplanningfortherestorationandreconstruction,strengtheningearthquakepreventionanddisasterreductionpropaganda,improvingtheawarenessofearthquakepreparednessintheagriculturalandpastoralareas,strengtheningtheguidanceandsupervisionofhousingconstructioninruralareastoreducethecasualtiesandlosses,andpromotingtheharmoniousdevelopmentofeconomyinTibet.
简介:目的探讨乙型肝炎病毒pre—S1Ag、pre—S2Ag、HBV—DNA、HBV—M的相关性及其临床意义。方法HBV—DNA采用荧光定量PCR法;HBV—M及pre—S1Ag、pre—S2Ag采用ELISA法,检测96例HBV—DNA阳性感染者血清中pre-S1Ag、pre—S2Ag、HBV—M,同时以30例HBV—M全阴性的健康体检者血清作为对照,并对结果进行统计学分析。结果96例HBV—DNA阳性患者中HBsAg、HBeAg、HBcAb阳性检出率为64.6%;HBsAg、HBeAb、HBcAb阳性检出率为20.8%;HBsAg、HBcAb阳性栓出率为14.6%;pre—S1Ag在96例HBV—DNA阳性标本中检出率为70.8%;pre—S2Ag检出率为79.2%;均明显高于HBeAg的阳性率64.6%,30例对照中未检测出pre—S1Ag、pre—S2Ag及HBV—DNA。结论HBeAg、HBV—DNA、pre—S1Ag、pre—S2Ag之间具有一定的关联性。pre—S1Ag和pre—S2Ag均较HBeAg敏感。pre—S1Ag与pre—S2Ag的栓出率差异无显著性,ELISA检测HBV—M、pre—S2Ag及pre—S1Ag只是表型指标,只能提供HBV感染的间接证据。而HBV—DNA的检测是HBV感染与否的直接证据。HBV—M、pre—S1Ag、pre—S2Ag、HBV—DNA的检测各自有其独特的临床意义。应用pre—S1Ag、pre—S2Ag、HBV—DNA及HBV—M进行联合检测,对HBV感染的早期诊断,了解HBV复制、转归及监测疗效和预后有重要的意义。
简介:Inthispaper,basedonGansuDigitalSeismicNetworkdatasince1990,wecalculatedb-valueand⊿b-valueoftheneighborhoodareabeforethe2013Minxian-ZhangxianM_S6.6,earthquake.Theresultsshowthattheearthquakeoccurredatthemarginofthesignificantlylowerb-valueareainsoutheastofGansuandbeforetheearthquaketheneighborhoodareahadanobviouslyabnormal⊿b-value.Fromtheearthquakeandthespatialdistributionoflowb-value,theregionstillhasthepossibilityofgeneratingdangerousstrongearthquakes.
简介:汶川Ms8.0级地震发生在青藏高原东缘著名的龙门山断裂带上,造成了中央断裂和前山断裂共约330kin的地震地表破裂带。初步研究表明,龙门山断裂带上大震复发可能属特征地震模式。结合龙门山断裂带的地震地质情况和汶川地震地表破裂带的基本参数综合分析,本文从地质学、地震学和GPS数据分析三个方面评估了龙门山断裂带的大震复发周期。结果表明,上述三种方法获得的龙门山断裂带Ms8.0级地震的复发间隔分别为:3185a、170(02264a和4310a,平均为3000a左右:Ms7.5级地震的平均复发间隔为1000a左右;Ms7.0级地震的平均复发间隔为500a左右。这些结果与其他学者的研究结果相比,相差不多,基本反映了龙门山断裂带的地震能量水平和累积速度。