资源描述:
《腾冲地体坡仑山岩体锆石U-Pb年龄和地球化学组成》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、2015年9月,第21卷,第3期,508-518页高校地质学报September2015,Vol.21,No.3,pp.508-518GeologicalJournalofChinaUniversitiesDOI:10.16108/j.issn1006-7493.2014130腾冲地体坡仑山岩体锆石U-Pb年龄和地球化学组成1121111*巫嘉德,王岩,谢清陆,齐玥,李俊辉,贺剑峰,陈福坤1.中国科学技术大学地球和空间科学学院,合肥2300262.海军蚌埠士官学校航海系,蚌埠233012摘要:滇西特提斯构造域广泛发育中—新生代岩浆作用,是长期复杂的造山作用的结果。出露于腾冲地
2、块的坡仑山花岗岩体锆石U-Pb年龄和地球化学特征显示,坡仑山岩体主要岩石类型为斑状花岗闪长岩,以全碱含量高为特征,属于高钾钙碱性系列,富集大离子亲石元素、亏损高场强元素(Nb、Ta、Ti和P)。锆石U-Pb定年结果指示岩体的侵位时代为66~63Ma,是新特提斯洋汇聚过程的产物。部分锆石颗粒或晶区具有高的U和Th含量特征,其U-Pb年龄集中在35~30Ma,明显年轻于岩体侵位时代,而与高黎贡山变质带变质—变形时代吻合,可能反映高U-Th锆石同位素体系遭受热事件重置。全岩Sr-Nd同位素组成显示富集特征,初始87Sr/86Sr比值介于0.7158和0.7164之间,初始εNd值为
3、-14.5至-15.3,对应Nd模式年龄值为2.04~2.10Ga,推测岩浆源区可能以古元古代地壳物质为主。关键词:特提斯带;腾冲;花岗岩;Sr-Nd-Pb同位素;锆石年龄中图分类号:P595文献标识码:A文章编号:1006-7493(2015)03-0508-011ZirconU-PbAgesandGeochemicalCompositionofthePolunshanPlutonintheTenchongBlock,WesternYunnan1121111*WUJiade,WANGYan,XIEQinglu,QIYue,LIJunhui,HEJianfeng,CHENFu
4、kun1.SchoolofEarthandSpaceSciences,UniversityofScienceandTechnologyofChina,Hefei230026,China;2.BengbuNavalPettyOfficerAcademy,DepartmentofNavigation,Bengbu233012,ChinaAbstract:MesozoictoCenozoicmagmaticactivities,widelydistributedintheTethyanbeltofwesternYunnan,areinducedbythelong-timecompl
5、icatedorogenicprocesses.ZirconU-PbagedataandgeochemicalcharacteristicsofthePolunshangranite,exposedintheTenchongblock,arereportedinthisstudy.ThePolunshangraniteplutoniscomposedmainlyofporphyriticcoarse-grainedgranodiorites.Geochemically,thisgraniteischaracterizedbyhighalkalicontentsandbelon
6、gstothehigh-potassiccalc-alkalinerocktype.Itenrichesinlarge-ionlithosphileelementsanddepletesinhighfield-strengthelements(Nb,Ta,TiandP).ResultsofthezirconU-Pbdatingsuggestemplacementagesof66~63Maforthemagma(s)ofthePolunshangranite,pointingtoamagmaticproductrelatedtotheclosureoftheNeo-Tethys
7、Ocean.ManyanalysedzircongrainsorcrystaldomainshavehighcontentsofUandTh.TheyyieldU-Pbagesofabout35~30Ma,significantlyyoungerthanemplacementtimeofthegranite,butsimilartotheageofdeformationormetamorphismoftheGaoligongshanmetamorphicbelt.Thisphanomenonimplie