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东昆仑那陵格勒河地区新元古代变质侵入体LA-ICP-MS锆石U-Pb年龄及意义

严玉峰 杨波 李焕学 才航加 许海全 许玉豪

西北地质2017,Vol.50Issue(4):33-40,8.
西北地质2017,Vol.50Issue(4):33-40,8.

东昆仑那陵格勒河地区新元古代变质侵入体LA-ICP-MS锆石U-Pb年龄及意义

Single-Zircon U-Pb and Geological Significance of Metamorphic and Intrusive System of NALINGELE Region in East Kunlun Neo-proterozoic

严玉峰 1杨波 2李焕学 1才航加 2许海全 1许玉豪2

作者信息

  • 1. 青海省地质调查院,青海西宁810012
  • 2. 青海省青藏高原北部地质过程与矿产资源重点实验室,青海西宁810012
  • 折叠

摘要

Abstract

Neo-proterozoic metamorphic and intrusive rocks (bodies) are discovered in Nalinggelehe area in East Kunlun,which were intruded into Jinshuikou Paleo-proterozic rock group and Wanbaogou Mesoproterozoic-Neoproterozoic rock group,with the lithology of granodioritic gneiss and monzonitic granitic gneiss.The LA-ICP-MS zircon dating of granodioritic gneiss has yielded an age of (840±2) Ma,which belongs to the Neo-proterozoic era.Rock geochemistry shows the characteristics of strong peraluminous,high potassium calc-alkaline series rock,with the features of S type granite,which was formedin continental collision orogenic environment and served as a product of the collision environment.This age and the available dating data suggest that a Meso-to Neo-Proterozoic granitic intrusive belt exists in the eastern margin of the Kunlun block,and that the whole Kunlun block might be a response to the amalgamation event of global Rodinia supercontinent.

关键词

新元古代/变质侵入体/花岗闪长质片麻岩/大陆碰撞造山

Key words

Neo-proterozoic/intrusive rock/granodioritic gneiss/continental collision orogeny

分类

天文与地球科学

引用本文复制引用

严玉峰,杨波,李焕学,才航加,许海全,许玉豪..东昆仑那陵格勒河地区新元古代变质侵入体LA-ICP-MS锆石U-Pb年龄及意义[J].西北地质,2017,50(4):33-40,8.

基金项目

中国地质调查局西安地质调查中心“青海1∶25万布伦台、大灶火幅区调修测”项目(1212011121187) (1212011121187)

西北地质

OA北大核心CSCDCSTPCD

1009-6248

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