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首页|期刊导航|地质通报|临沧地体亲缘性及南段组物源——来自泥盆纪—石炭纪南段组碎屑锆石U-Pb年龄的证据

临沧地体亲缘性及南段组物源——来自泥盆纪—石炭纪南段组碎屑锆石U-Pb年龄的证据

曾文涛 刘桂春 冯庆来 赵天宇 俞赛赢 邓仁宏 莫熊

地质通报2017,Vol.36Issue(7):1175-1187,13.
地质通报2017,Vol.36Issue(7):1175-1187,13.

临沧地体亲缘性及南段组物源——来自泥盆纪—石炭纪南段组碎屑锆石U-Pb年龄的证据

The relationship between Lincang block and prove?nance of Nanduan Formation: Evidence of detrital zircon U-Pb dating from metasandstone of Devonian-Carboniferous Nanduan Formation

曾文涛 1刘桂春 1冯庆来 2赵天宇 2俞赛赢 2邓仁宏 1莫熊1

作者信息

  • 1. 云南省地质调查院,云南 昆明 650216
  • 2. 中国地质大学地质过程与矿产资源国家重点实验室,湖北 武汉 430074
  • 折叠

摘要

Abstract

Absract:U-Pb ages of detrital zircons of Devonian-Carboniferous Nanduan Formation from Lincang block define three distinctive age peaks in older Grenvillian (1100~1300Ma), younger Grenvillian (900~980Ma) and Pan-African (530~680Ma), and two subordi?nate group in 1550~1730Ma and 2350~2630Ma, suggesting that the provenance of sediments had multi-source and complex charac?teristics. The age spectrum is obviously different from detrital zircon age spectrum of the Devonian-Carboniferous sediments of Si?mao block, which indicates that the sediments of Nanduan Formation came from East Ganwana supercontinent, and the result is indi?cated by paleobiology which shows a genetic relationship between East Ganwana and paleo-Tethys in southwest Yunnan.

关键词

碎屑锆石/LA-ICP-MSU-Pb年龄/物源分析/碎屑岩/南段组/临沧地体/滇西南

Key words

detrital zircon/LA-ICP-MS U-Pb age/provenance analysis/metasandstone/Nanduan Formation/Lincang block/southwest Yunnan

分类

天文与地球科学

引用本文复制引用

曾文涛,刘桂春,冯庆来,赵天宇,俞赛赢,邓仁宏,莫熊..临沧地体亲缘性及南段组物源——来自泥盆纪—石炭纪南段组碎屑锆石U-Pb年龄的证据[J].地质通报,2017,36(7):1175-1187,13.

基金项目

中国地质调查局项目《云南区域地质调查片区总结与服务产品开发》(编号:DD20160345-02)、国家自然科学基金项目《滇西南原题特斯及其与古特提斯演化关系研究》(批准号:41672222)和云南省科技基金项目《西南"三江"叠合成矿作用与成矿预测》(编号:2013HA001) (编号:DD20160345-02)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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