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青海东昆仑东段塔妥地区小庙岩组变质岩LA-ICP-MS锆石U-Pb年龄及其地质意义

王旭斌 邓文兵 裴先治 李瑞保 陈有炘 刘成军 李佐臣 杨森 桑继镇 陈功

地质通报2016,Vol.35Issue(7):1144-1157,14.
地质通报2016,Vol.35Issue(7):1144-1157,14.

青海东昆仑东段塔妥地区小庙岩组变质岩LA-ICP-MS锆石U-Pb年龄及其地质意义

LA-ICP-MS zircon U-Pb ag-es of metamorphic rocks from Xiaomiao Formation in Tatuo area of eastern East Kunlun Mountains and their geological sig-nificance

王旭斌 1邓文兵 1裴先治 1李瑞保 2陈有炘 1刘成军 2李佐臣 1杨森 1桑继镇 1陈功2

作者信息

  • 1. 长安大学地球科学与资源学院,陕西西安710054
  • 2. 西部矿产资源与地质工程教育部重点实验室,陕西西安710054
  • 折叠

摘要

Abstract

There has been long controversy over the formation age of the Xiaomiao Formation in the eastern part of East Kunlun oro⁃genic belt due to the lack of precise age. Choosing the meta-detrital rocks of Xiaomiao Formation in Tatuo area in eastern East Kun⁃lun orogenic belt as the study objects, the authors used LA-ICP-MS zircon U-Pb isotope geochronologic method to study the for⁃mation age of Xiaomiao Formation. The result shows that it has a wide age range (1551~2624Ma) which can be evidently divided in⁃to four groups, namely 2624~2603Ma, 2501~2290Ma, 2196~2036Ma and 1921~1551Ma, and the last group can be further divided into two subgroups of 1921~1690Ma and 1641~1551Ma. The age range 1921~1690Ma with the most intense peak value of 1783Ma represents a metamorphism and magmatism of the source region whereas the age range 2501~2290Ma represents a metamorphism of the source region. The detrital zircon also has the age range 2196~2036Ma with some detrital zircons being 2600Ma, which implies that there exists a Neoarchean basement in East Kunlun. The age range 1641~1551Ma (weighted average age equal to 1597Ma) repre⁃sents the metamorphism time of Xiaomiao Formation, and the latest metamorphism age of the source region is 1690Ma, which re⁃stricts the formation age of Xiaomiao Formation, which should belong to Mesoproterozoic. The contrast of the metasedimentary zir⁃con age range and metamorphosed basement tectonic-thermal event of the East Kunlun Mountains shows that the main sediments of Xiaomiao Formation were from Mesoproterozoic Baishahe Formation, and East Kunlun area and North China Craton have similar tectonic evolution processes from the end of Paleoproterozoic to the beginning of Mesoproterozoic, as shown by contrasting their tec⁃tonic-thermal events.

关键词

东昆仑/LA-ICP-MS锆石U-Pb年龄/小庙岩组/中元古代

Key words

East Kunlun Mountains/LA-ICP-MS zircon U-Pb age/Xiaomiao Formation/Mesoproterozoic

分类

地质学

引用本文复制引用

王旭斌,邓文兵,裴先治,李瑞保,陈有炘,刘成军,李佐臣,杨森,桑继镇,陈功..青海东昆仑东段塔妥地区小庙岩组变质岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质通报,2016,35(7):1144-1157,14.

基金项目

国家自然科学基金项目(批准号:41472191、41502191、41172186)、高等学校博士学科点专项科研基金项目(编号:20110205110004)和中央高校基本科研业务费专项资金项目 ()

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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