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柴达木地块南缘昆北单元变质新元古代花岗岩锆石SHRIMPU-Pb年龄
引用本文:陈能松,李晓彦,王新宇,陈强,王勤燕,万渝生.柴达木地块南缘昆北单元变质新元古代花岗岩锆石SHRIMPU-Pb年龄[J].地质通报,2006,25(11):1311-1314.
作者姓名:陈能松  李晓彦  王新宇  陈强  王勤燕  万渝生
作者单位:1. 中国地质大学地球科学学院,湖北,武汉,430074
2. 中国地质大学地球科学学院,湖北,武汉,430074;广西地质调查院,广西,南宁,530023
3. 北京离子探针中心,北京,100037
基金项目:教育部科学技术研究重点项目,国家自然科学基金
摘    要:侵入于香日德南昆北单元金水口岩群白沙河岩组中的变质花岗岩的锆石SHRIMP U-Pb年龄约为904Ma.该年龄与东昆仑地区已有的定年数据一道,表明柴达木地块南缘存在一条中-新元古代的花岗岩深成侵入岩带,整个柴达木地块可能曾响应了全球Rodinia超大陆汇聚事件.

关 键 词:变质花岗岩  锆石SHRIMP  U-Pb定年  Rodinia超大陆汇聚  柴达木地块南缘
文章编号:1671-2552(2006)11-1311-04
收稿时间:2006-04-29
修稿时间:8/9/2006 12:00:00 AM

Zircon SHRIMP U-Pb age of Neoproterozoic metagranite in the North Kunlun unit on the southern margin of the Qaidam block in China
CHEN Neng-song,LI Xiao-yan,WANG Xin-yu CHEN Qiang,WANG Qin-yan,WAN Yu-sheng.Zircon SHRIMP U-Pb age of Neoproterozoic metagranite in the North Kunlun unit on the southern margin of the Qaidam block in China[J].Geologcal Bulletin OF China,2006,25(11):1311-1314.
Authors:CHEN Neng-song  LI Xiao-yan  WANG Xin-yu CHEN Qiang  WANG Qin-yan  WAN Yu-sheng
Institution:1. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China; 2. Guangxi Institute of Geological Survey, Nanning 530023,Guangxi, China; 3. Beijing SHRIMP Center, Beijing 100037 ,China
Abstract:Zircon from a metagranite pluton in the Baishahe Formation of the Jinshuikou Group in the North Kunlun unit yields a SHRIMP U-Pb age of ca. 904 Ma. This age and the available dating data suggest that there exists a Meso- to Neoproterozoic granitic intrusive belt on the southern margin of the Qaidam block and that the whole Qaidam block probably regionally responded to the amalgamation event of the global Rodinia supercontinent.
Keywords:metagranite  zircon SHRIMP U-Pb dating  amalgamation of the Rodinia supercontinent  southern margin of the Qaidam block
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