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1、中國(guó)地質(zhì)科學(xué)院碩士學(xué)位論文滇藏鐵路金沙江河谷段工程地質(zhì)條件研究姓名:郭長(zhǎng)寶申請(qǐng)學(xué)位級(jí)別:碩士專業(yè):地質(zhì)工程指導(dǎo)教師:張永雙20070120中國(guó)地質(zhì)科學(xué)院碩士學(xué)位論文ABSTRACTTheYunnan幣betrailwayisoneofthemostimportantplanningrailwaysofChinaAndithasbeenapartodtoseveralsubsectionsandeachsubsectionwillbeco
2、nstructedindividiualyTheJinshaRivervalleywhichisontherouteoftheLijiang—ShangrilasubsectionandthegeologicalconditionsarecomparativelycomplexHowto州dgingoverandwheretolocatethebridgearcthekeyissueswhichrestricttherallwayori
3、entationTherefore,thisstudyselectstheJinshaRivervalleyasthestudyareaandappliesmultisubjectstheoriesandmethodstoasseSStheJinshaRivervalleygeologicalconditionsandanalysesthcslopestabilityofthepotentialbridgelocationaswellB
4、asedontheanalysisoftheregionalgeologicalbackgroundthispaperreviewsthefeaturesoftheneotectonicmovementsandmainactivefaultsinthestudyareaandrevealsthattheZhongdianfaultandtheLongpanQieohoufaultare協(xié)emainactivefaultswhichtos
5、omeextentaffecttheJinshaRiverBridgeproject11他analysesofthetopographyfeaturesgeologicalandhydrogeologicalconditionsandtheGeohazatdsdistributionofthewholestudyareaindicatesthattheengineeringgeologicalconditionsoftheXialuoy
6、uBridgeoeattheShangxiakouoftigerleapinggorgeisrelativebetterThispaperlucubratethestabilityofthehighslopesofthevalleyandtheLengducomplexslopebodywhichaffectthebridge嘶Engineeringgeologicalanalysisandtheelasticplasticfinite
7、elementsimulationresultsindicatethat:1)ThereisplasticzoneintheIeftvalleybottomslopewiththeeffectsofgravityandearthquakeandthereissmallplasticargoatthelowerpartoftherightvalleyloosedebris;2)Whentheportentialderwnraverre∞r(nóng)
8、voirwereonthehighwaistleveltheplasticloeationeoncon懈intheIeftsideatthevicinityofthesamehightofthewaterlevel111eLeogducomplexslopebodycanbedividedintothreepaffs:theslopesectionfromtheShan鰣LaNo3higIlschooltotheestuarythean
9、cientlandslidesectionfromChangshangt0HezanandthebedrocksectionattheNortheastofShibuge111eauthorcalculatesandanalysesthestabilityoftheancientlandslidesectionfromChangshengtoHezanusingtheSwedishslicemuthodJanbumethodandthe
10、simplifiedBishopmethod,withtheconditionsofthecurrentstatus,carthquakewaterstorageandrainfallI矗equantitativecalcdationresultsshowthattheancientlandslidesisstableandofhigllreliabilitywiththesafIycoefficientof1257一1413incur
11、rentstatus,andthestahilitydecre笛etoO92虬1043and0960一13l5undertheconditionofrainfalland7—9degreeearthquakewhilenlesaltycoe最cientturnto0861to0,960underthecombinedofearthquakeandrainfajlandthismeansunstabi|ityInordertovalida
12、tetheabovementionedresultstheslicenumaricaJsolutionmethodandtheMonteCatlosimulationmethodwerecombinedtocalculatethestabilityoftheChangshengHezanancientlall出lideTheabovecoleulationandanalysisrevealthattheselectedIocatlono
13、fXialuoyuBridgeisappropriatewithrespecttotheen百neeringgeologicalconditionsInordert0guidetherailwayplanningandengineeringgeologicalsurveythispapercarryouttheellgl’neeringgeologicalconditionzonationassumedtheJinshaRiverBri
14、dgelocationweredecided,ApplyingAnalyticalHierarchyProcessandGIS,whichbaseontheplatformofMapGIS67andArcGIS91Andterrainslopeengin∞r(nóng)inggeologicalrockgroups,slopestructure,theGeehazardsdistribution,earthquakepeakacceleration
15、activefaulttinyphysiognomyhumanactivityrainfall(maindifferencesinvertical)andthedistancetothedraingeswereselectedasindicesandquantifiedwithexpefcopinionsforthezonatiooAccordingtotheGIScalculationthestudyatgaisdividedinto
16、4engineeringgeologicalclasses:besLbettermiddleandpoorAccording|0thezonationtheXialuoyuBridgemainlybridgeoverthebetterengineeringgeologicalareaandthemiddleengineeringgeologicalareawhichprovesthattheformeranalyaisandcal吼na
17、ti013a北reasonableThetechniquesandmethodelegyusedinthisstudycanbereferencedwhenstudyingthesimilarengineeringgeologicalsubjeclsinotherregionsKeyWords:Yunnan—TibetRailwaytheJinshaRiverValleyHi|ghSlope,ComplexSlope,Engineeri
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