华北地质2024,Vol.47Issue(3) :14-22,35.DOI:10.19948/j.12-1471/P.2024.03.02

坦桑尼亚卢帕地体花岗岩岩石地球化学特征、锆石U-Pb年代学及其构造意义

Geochemical characteristics,Zircon U-Pb isotopic and the indicative geotectonic environment of the granitoids in Lupa terrain,Tanzania

何胜飞 刘晓阳 孙凯 许康康 龚鹏辉
华北地质2024,Vol.47Issue(3) :14-22,35.DOI:10.19948/j.12-1471/P.2024.03.02

坦桑尼亚卢帕地体花岗岩岩石地球化学特征、锆石U-Pb年代学及其构造意义

Geochemical characteristics,Zircon U-Pb isotopic and the indicative geotectonic environment of the granitoids in Lupa terrain,Tanzania

何胜飞 1刘晓阳 1孙凯 1许康康 1龚鹏辉1
扫码查看

作者信息

  • 1. 中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170;中国地质调查局南部非洲矿业研究所,天津 300170
  • 折叠

摘要

[研究目的]卢帕地体是坦桑尼亚第二大金矿集区所在地,对于其形成时代及成因机制争议较大.[研究方法]本次通过锆石年代学和地球化学特征分析,厘定卢帕地体花岗岩的形成时代和成因机制.[研究结果]锆石U-Pb年代学研究表明卢帕地体内花岗岩有两类:新太古代花岗岩类,年龄为2 663±22 Ma~2 778±13 Ma;古元古代花岗岩年龄为1 944±10 Ma~2 006±10 Ma,地球化学特征与I型花岗岩相似.卢帕地体内分布的其它基性岩、碳酸岩等代表了罗迪尼亚超大陆裂解开始的时间.[结论]岩石地球化学特征表明非A型花岗岩,其物质来源并非来自地幔,而是地壳重熔的结果.花岗岩构造环境判别图解显示,样品投影落在火山弧花岗岩中,花岗岩集中于大陆花岗岩区域,远离大洋花岗岩、大洋玄武岩和辉长岩区域,新太古代与古元古代的花岗岩形成于大陆边缘弧.

Abstract

[Objective]Lupa terrane is the second largest gold ore concentration area in Tanzania,and its formation age and genetic mechanism are controversy.[Methods]Through the analysis of zircon geochronology and geochemical characteristics of granite,the formation age and genetic mechanism of the Lupa terrane granite are determined.[Results]Zircon U-Pb geochronology studies indicate that there are two types of granites in the Lupa terrane:Neoarchean granites(2 663±22 Ma~2 778±13 Ma);Paleoproterozoic granite(1 944±10 Ma~2 006±10 Ma),and their geochemical characteristics are similar to those of I-type granite.The other basic rocks,carbonates and other rocks distributed within the earth represent the beginning of the breakup of the Rodinian super continent.[Conclusions]The geochemical characteristics of rocks indicate that the material source of non-A-type granite is not from the mantle,but the result of crustal remelting.The tectonic environment discrimination diagram of the granite shows that the sample projection falls in the volcanic arc granite,and the granite is concentrated in the continental granite area,away from the oceanic granite,oceanic basalt and gabbro area.The Neoarchean and Paleoproterozoic granites were formed in the continental margin arc.

关键词

锆石U-Pb年代学/地球化学特征/卢帕地体/坦桑尼亚

Key words

Zircon U-Pb geochronology/geochemical characteristics/Lupa terrane/Tanzania

引用本文复制引用

出版年

2024
华北地质
天津地质矿产研究所

华北地质

影响因子:0.61
ISSN:1672-4135
段落导航相关论文