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首页|期刊导航|地质学报(英文版)|Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform

Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform

侯增谦 陈文 卢记仁

地质学报(英文版)2002,Vol.76Issue(2):194-204,11.
地质学报(英文版)2002,Vol.76Issue(2):194-204,11.

Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform

Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform

侯增谦 1陈文 2卢记仁3

作者信息

  • 1. Institute of Mineral Resources, Chinese Academy of Geological Sciences Beijing, 100037
  • 2. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037
  • 3. 3College of Earth Sciences, China University of Geosciences, Beijing 100029
  • 折叠

摘要

Abstract

Geochronology of continental flood basalts sampled from the Emei large igneous province (LIP) on the western margin of the Yangtze platform was investigated by the laser microprobe 40Ar/39Ar dating technique. These basalts yield a fairly wide range of 40Ar/39Ar ages, varying from 259 to 135 Ma. One basalt sample, at least altered, recorded the oldest 40Ar/39Ar age of about 259 Ma, corresponding to a peak eruption age of the Emei LIP continental flood basalts. Most of the samples yield much younger ages from 135 to 177 Ma, which are consistent with the K-Ar ages for the same samples (122.8-172.1 Ma). The dating data suggest that these Permian basalts had been widely affected by the regional tectonothermal event at 177-135 Ma. The event was probably caused by the convergence and collision among the Laurasia, Yangtze and Qiangtang-Qamdo continental blocks on the eastern margin of the Qinghai-Tibet plateau after the late Triassic. The age of the event reflects the timing of the peak collisional orogeny.

关键词

40Ar/39Ar age, basalts in the Emei LIP, collisional orogeny, Qinghai-Tibet plateau

Key words

40Ar/39Ar age, basalts in the Emei LIP, collisional orogeny, Qinghai-Tibet plateau

分类

天文与地球科学

引用本文复制引用

侯增谦,陈文,卢记仁..Collision Event during 177-135 Ma on the Eastern Margin of the Qinghai-Tibet Plateau: Evidence from 40Ar/ 39Ar Dating for Basalts on the Western Margin of the Yangtze Platform[J].地质学报(英文版),2002,76(2):194-204,11.

基金项目

This study was supported by the Youth Foundation of the Ministry of Land and Resources and the National Natural Science Foundation of China (Grant 49973003). The authors thank the anonymous reviewers for their constructive comments and suggestions. (Grant 49973003)

地质学报(英文版)

1000-9515

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