九寨沟风景区的表生地球化学特征(supergene geochemical characteristics of jiuzhaigou scenic area)

九寨沟风景区的表生地球化学特征(supergene geochemical characteristics of jiuzhaigou scenic area)

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时间:2018-08-30

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1、九寨沟风景区的表生地球化学特征(SupergenegeochemicalcharacteristicsofJiuzhaigouScenicArea)LuozhengchunAbstract:Jiuzhaigouscenicspotenjoysagoodreputationbothathomeandabroadforitsspecialnaturalscenery.Inthispaper,thegeochemicalenvironmentofthesupergenegeochemistryisdiscussedfromtheview

2、ofgeochemistry,whichprovidesreferenceforfurtherdevelopmentandprotectionofthearea.Keywords:Jiuzhaigou;geochemistry;supergeneenvironmentClassificationnumber:P59:X142documentidentificationcode:AArticlenumber:1001-1749(2000)01-0048-04SURFACEGEOCHEMICALNATUREOFSCENICSPOT,J

3、IUZHAIVALLEYLUOZheng-chun(GeochemicalTeamofSichuanMinistryofGeologyandMineralResources,Sichuan,618009,China)Abstract:ScenicspotofJiuzhaiValleyinSichuanprovinceofChinahasthegoodreputationinthecountryandoverseasforitsspecificnaturescenery.Inthispaperwewillgiveoriginalde

4、scriptionofgeochemicalmechanismintheviewofgeochemistryenvironments,andofferanusefulreferenceforfurthertouristdevelopmentandenvironmentprotectioninthissceneryarea.Keywords:jiuzhaivalley;geochemistrysurface;environment0naturalgeographysurveyJiuzhaigouhighandcoldmountain

5、karstlandscapearea,locatedinJiuzhaigouCountyofNorthwestSichuanPlateau,isawhiteLongjiangRiverBasin,borderingonthesourceofMinjiangRiversystem.3000~4700mabovesealevel.Rainfallisabundant,andtheannualaverageprecipitationis649.6~940.6mm.Moderateclimate,annualminimumtemperat

6、urefor20.6DEGC,themaximumtemperatureof30degreesC.Thescenicnaturalscenery,vegetationdevelopment,verticalzoning,alpinevalleytravertineSnowgleamswhite.widecloth,color,colorful,beautiful,scenicspotstogetherisararespectacularnaturallandscapemasterpiece.1GeologicalprofileLo

7、catedinthewesternQinlingMountainsgeosynclinefoldbeltFerrisrangeanticline,thestrataofDevonianinthickbeddedlimestone,dolomiticlimestoneandslate;Carboniferouscrystallinelimestone,dolomiticlimestoneandclayshale;blackPermianlimestoneandshale;thelowerTriassicdolomiticlimest

8、one.ThestrataaregenerallyNWtrending.TheNWtrendingandNEtrendingfaultsdevelopedinthearea,andhadcertaincontroloverthescenicspot

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