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时间:2017-12-08
《库鲁克塔格地区新元古代沉积物源分析_来自碎屑锆石年代学的证据_张英利》由会员上传分享,免费在线阅读,更多相关内容在教育资源-天天文库。
1、1000-0569/2011/027(01)-0121-32ActaPetrologicaSinica岩石学报库鲁克塔格地区新元古代沉积物源分析:来自碎屑*锆石年代学的证据11222张英利王宗起闫臻王涛郭现轻11222ZHANGYingLi,WANGZongQi,YANZhen,WANDTaoandGUOXianQing1.中国地质科学院矿产资源研究所,北京1000372.中国地质科学院地质研究所,北京1000371.InstituteofMineralResources,ChineseAcademyofGeologicalS
2、ciences,Beijing100037,China2.InstituteofGeology,ChineseAcademyofGeologicalSciences,Beijing100037,China2010-04-18收稿,2010-04-29改回.ZhangYL,WangZQ,YanZ,WangTandGuoXQ.2011.ProvenanceofNeoproterozoicrocksinQuruqtagharea,Xinjiang:Evidencefromdetritalzircongeochronology.Act
3、aPetrologicaSinica,27(1):121-132AbstractTheQuruqtaghareaissituatedinthelinkageofSouthTianshanandTarimbasinwherewellpreservedsedimentaryrecords.TheBeiyixiFormationintheQuruqtaghareaisavolcanic-sedimentarysuccessionwhichconsistsofigneousrocksandsandstones.TheYukengouF
4、ormationischaracterizedbysandstonesandsiltstonesformedbyturbiditycurrent.DetritalzirconU-PbagesoftwosamplesfromthesandstonesweremeasuredbytheLA-ICP-MSmethod.Thesample09DPL25and09DPL41respectivelyrecords93and71agedata.Detritalzirconsofsample09DPL25fromBeiyixiFormatio
5、nwhosepeakageis821Maandsubordinatepeakageis861Maareprevalent.Andthemajorityofdetritalzirconsofsample09DPL41fromYukengouFormationisweighted-age768Ma(subordinate800Maand741Ma).BasedonCLimages,thereoccurredafewmagmaticeventsabout741Ma,768Ma,821Maand861Ma.Togetherwithth
6、eliteraturedata,itstronglysuggeststhatthebasementrocksintheQuruqtaghregionwereformedintheMeso-toNeo-Archeanperiod.DetritalzirconsindicatethattheprovenancesofBeiyixiFormationare761~847Ma,851~972Maand1808~2498MarocksandmainprovenanceagesofYukengouFormationare734~845Ma
7、,858~963Maand1708~2486Ma.KeywordsDetritalzircon;U-Pbgeochronology;Provenance;Quruqtagh摘要库鲁克塔格位于南天山和塔里木盆地接合部,保留相对较完整的地层记录。新元古代贝义西组主要为一套火山-沉积组合序列,育肯沟组为浊流成因的砂岩和粉砂岩组合。对取自两个地层的沉积岩样品,分别进行了碎屑锆石LA-ICP-MSU-Pb测年,并分别获得了93组和71组U-Pb有效年龄。其中贝义西组锆石U-Pb年龄主峰值为821Ma、次峰值为861Ma的碎屑锆石(761
8、~847Ma)具有显著优势,育肯沟组年龄值为768Ma(次峰值为800Ma和741Ma)的碎屑锆石比较集中,说明库鲁克塔格地区在741Ma、768Ma、800Ma、821Ma和861Ma有大规模的岩浆活动。10个太古代碎屑锆石年龄以及综合已有的研究成果,确认库鲁克塔格存在中-
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