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ID:32073719
大小:10.53 MB
页数:100页
时间:2019-01-31
《松潘—甘孜造山带东部金川地区黄岗岩类地质地球化学特征与构造背景》由会员上传分享,免费在线阅读,更多相关内容在学术论文-天天文库。
1、西南科技大学硕士研究生学位论文第1II页AbstractSongpan—Garzefoldbelt,locatedinthenortheasternmarginoftheTibet.anplateau,asthemaintectonicconvergencezoneofthenorthChinaplateandtheYangtzeplate,theQiangtangblock,underwenttwophasesoforogenesis:Paleo-TethysandNeo-Tethys,thetectonicevolutionprocessofcomplex,calle
2、d”Chinesegeologicalbermuda”.Acidicgranitoidswidelyexposedinthezone,forthesegranitoidemplacementage,petrolgeochemcharacteristics,rockformationmechanismandtectonicbackgroundandotherissuesofresearch,torevealtheSongpan·Garzefoldbeltcomplexgeologicalevolutionanditsdymamicmechanismhasimportants
3、cientificsignificance.Therefore,thepaperselecttherelativelyweakresearchofErmaomountain,Wanlicheng,Kongkaliangzi,DusongfourrockastheresearchobjectofJinchuanarea,easternoftheSongpan-Garzefoldbelt,onthebasisoffieldgeologicalinvestigation,tostudyindetailthecharacteristicsofpetrology,zirconu-p
4、bgeochronologyandgeochemistry,combinedwiththepreviousresearchresults,discussestheformationmechanismofthegranitoidsintheresearchareaandthetectonicenvironment.Obtainthefollowingresultsandunderstanding:(1)UsingtheLA-ICP-MSzirconu-pbdatingoffourrockoftheresearcharea,determinationofErmaomounta
5、inbiotitegraniteattheageof206.4+4.5Ma.Wanlichengbiotitegraniteagerespectivelyis209.24-4.2Ma,210土4.6Ma;biotitequartz-syeniteageis206士2.7Ma,indicatethatbiotitegraniteearlieremplacementofbiotitequartz-syenite.Kongkaliangzisyenograniteageis215.8土2.4Ma.Dusongadamelliteageis199.0士2.3Ma.Eachrock
6、formationageissimilar,showingthattheymaybeformedonauniformdeepgeodynamicprocesses.Inaddition,thereareproterozoicinheritedzirconintheErmaomountainandWanlichengrock,andthencombinedwiththeresultsofpreviousstudiesshowthatthelowerpartoftheSongpan-Garzefoldbeltmaybeexistencecontinentalcrustalba
7、sement,whichsamewiththeYangtzeblockbasement.(2)Geochemicalanalysisresultsshowthat,Ermaomountainrockastheperaluminoushigh-kcalcalkalinerocks.IntheWanlichengrockbiotitegraniteandadamelliteforperaluminousKcalc-alkalinerocks;syenitemonzoniteofpartialaluminium..weakperal
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