21873.云南千湖山第四紀(jì)冰川作用與環(huán)境演變_第1頁(yè)
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1、遼寧師范大學(xué)碩士學(xué)位論文云南千湖山第四紀(jì)冰川作用與環(huán)境演變姓名:劉亮申請(qǐng)學(xué)位級(jí)別:碩士專業(yè):第四紀(jì)地質(zhì)學(xué)指導(dǎo)教師:張威201206云南千湖山第四紀(jì)冰川作用與環(huán)境演變QuaternaryGlaciationsdIheEnvironmelltalEvollltioninQianhuMountainofYunnanProvinceAbstractTheQianhuMountain,oneofthedefinitedistrictwherepr

2、eservedQuatemaryglacialremainsintheHengduanMountains,isintensivelyinfluencedbythesouthwesternmonsoonandhastheimportantscientificsignificanceintheresearchnotonlyonglacialcharacteristicsinwesternandeastemChina,butalsoonthe

3、relationshipbetweentheclimatechangeandtectonicupliftintheborderingmountainsofeasternTibetanPlateauFieldinvestigationfoundthattheQuatemauryerosionandsedimentgeomorphologyarepreservedabove3500minthemainpeakoftheQianhuMount

4、ainsanditssurroundingareasGlaciersmainlydependedontheplanationsurface(39004000m)andtherelativevalleyandtheglaciertypebelongstothesmallicecapandthevalleyglacierenteredthebranchvalleyUsinggeomorphologymethodandthelaboptica

5、llystimulatedluminescence(OSL)datingofglacialperiods,thispaperconfirmstheglacialadvanceonlytookplaceduringthelastglacialcycle(LGM),thatis,lastglacialmaximum(LGM,22219kaBP)inthemidlastglacialcycle(MIS3b,37337kaBP45643kaBP

6、),andintheearlystageoflastglacialcycle(MIS4)TheglacialextentoftheMIS3bislargerthanthatoflastglacialmaximumThismaybecausedbythedifferentclimatealternatedwithwetanddryclimateduringthedifferentglacialstageBasedonthemeasurem

7、entofenvironmentalsusceptibilityandanalysesofmagneticsusceptibilityofthemoraineaswellascomparedwithotherdataintheborderingmountainsofeasternTibetanPlateau,wemayconcludethatthemotherlithologichasaprimaryeffectonthemagneti

8、csusceptibilityvaluesoftheglacialdeposits,themainlithologicofQianhuMountainislimestone,themassmagneticsusceptibilityandthefrequencymagneticsusceptibilityislowerthanthatinLaojunMountainwhichconsistofgraniteandaslargeastha

9、tinShikaxueMountainwhichhasthesimilarlithologic,howeverthedifferenceofthevaluefromHelanMountainisnotonlyduetothelithologybutalsotheweatheringeffectinthelaterstageAccordingtotherelationshipbetweenthesmnmerJune,JulyandAugu

10、sttheannualprecipitationandtheatmospherictemperatureattheequilibriumlinealtitude,thepresentELAinQianhuMountainwas5322100mApplytheterminaltosummitaltitudinal(TSAM)tocalculatethepaleo—ELA,combinedwithtectonicuplift,weconcl

11、udethatthevalueis4003m、3954mand3835mrespectivelycorrespondingtothelastglacialmaximum,themiddlestageofthelastglacialcycleandtheearlystageofthelastglacialcycleComparedwiththemultiglaciersequenceintheHengduanMountains,Qianh

12、uMountainonlyexperiencedtheglacialadvanceduringthelastglacialcycleItisthetectonicupliftcoupledwiththeclimatechangethatledtheQianhumountaintothesnowlineandtookplacetheglacialadvanteKeywords:QianhuMountain;lastglacialcycle

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