| 注册
首页|期刊导航|现代地质|江南造山带东段赣东北蛇绿岩的形成时代:来自辉长岩LA-ICP-MS锆石U-Pb年龄的证据

江南造山带东段赣东北蛇绿岩的形成时代:来自辉长岩LA-ICP-MS锆石U-Pb年龄的证据

蒋幸福 彭松柏 KUSKY Timothy 王璐 邓浩 王军鹏

现代地质2017,Vol.31Issue(4):697-704,745,9.
现代地质2017,Vol.31Issue(4):697-704,745,9.

江南造山带东段赣东北蛇绿岩的形成时代:来自辉长岩LA-ICP-MS锆石U-Pb年龄的证据

Formation Time of the Northeastern Jiangxi Ophiolite in the Eastern Jiangnan Orogenic Belt: Evidence from LA-ICP-MS Zircon U-Pb Dating of the Gabbro

蒋幸福 1彭松柏 2KUSKY Timothy 2王璐 3邓浩 3王军鹏4

作者信息

  • 1. 东华理工大学地球科学学院,江西南昌330013
  • 2. 中国地质大学(武汉)地球科学学院,湖北武汉430074
  • 3. 中国地质大学(武汉)地质过程与矿产资源国家重点实验室,湖北武汉430074
  • 4. 中国地质大学(武汉)教育部长江三峡库区地质灾害研究中心,湖北武汉430074
  • 折叠

摘要

Abstract

Proterozoic Ophiolite of the eastern Jiangnan orogenic belt in Northeastern Jiangxi was mainly composed of serpentinized ultramafic rock,cumulated rock,isotropic gabbro and diabase,low-temperature and high-pressure blueschist and plagiogranite.LA-ICP-MS zircon U-Pb dating for one gabbro sample from the Northeastern Jiangxi Ophiolite yielded a 207pb/206pb age of (992 ± 25) Ma (MSWD =1.19),which represented the intrusion time of the gabbro.The geochronological result suggests the existence of Early Proterozoic palaeooceanic basin in the southeastern Yangtze block,which is younger than the late Meso-Proterozoic oceanic basin in the northern margin of the Yangtze block.Therefore,it is proposed that the Meso-Neoproterozoic crystallization basement rocks in the Yangtze craton were formed in a gradually aggregated process with characteristics of trending from northwest to southeast direction.

关键词

江南造山带/赣东北蛇绿岩/辉长岩/锆石U-Pb定年/新元古代早期

Key words

Jiangnan orogenic belt/Northeastern Jiangxi Ophiolite/gabbro/zircon U-Pb dating/Early Neoproterozoic

分类

天文与地球科学

引用本文复制引用

蒋幸福,彭松柏,KUSKY Timothy,王璐,邓浩,王军鹏..江南造山带东段赣东北蛇绿岩的形成时代:来自辉长岩LA-ICP-MS锆石U-Pb年龄的证据[J].现代地质,2017,31(4):697-704,745,9.

基金项目

国家自然科学基金项目(41272242) (41272242)

江西省教育厅科技项目(GJJ150562) (GJJ150562)

东华理工大学博士启动基金项目(DHBK2015321). (DHBK2015321)

现代地质

OA北大核心CSCDCSTPCD

1000-8527

访问量3
|
下载量0
段落导航相关论文