首页 | 本学科首页   官方微博 | 高级检索  
     检索      

江汉盆地河流碎屑锆石U-Pb年龄特征及其对物源研究的启示
引用本文:林旭,吴中海,赵希涛,张洋,陈济鑫,刘海金.江汉盆地河流碎屑锆石U-Pb年龄特征及其对物源研究的启示[J].地球学报,2022,43(1):73-81.
作者姓名:林旭  吴中海  赵希涛  张洋  陈济鑫  刘海金
作者单位:三峡大学土木与建筑学院;中国地质科学院地质力学研究所;中国科学院地质与地球物理研究所;东华理工大学地球科学学
基金项目:国家自然科学基金项目(编号: 41972212)
摘    要:江汉盆地位于扬子板块北部,是长江演化研究的关键地区.锆石是河流沉积物中常见的副矿物,其U-Pb年龄谱对比被广泛用于物源示踪研究,但在江汉盆地还未系统研究.本文利用激光剥蚀电感耦合等离子质谱(LA-ICP-MS)分别对江汉盆地12条流入河流进行了922颗碎屑锆石U-Pb年龄分析,结合多维判别图(MDS)和已报道的河流碎屑...

关 键 词:江汉盆地  锆石  U-Pb年龄  物源示踪

Detrital Zircon U-Pb Age Characteristics of Main Rivers around Jianghan Basin and Implications of Provenance Tracing
LIN Xu,WU Zhong-hai,ZHAO Xi-tao,ZHANG Yang,CHEN Ji-xin,LIU Hai-jin.Detrital Zircon U-Pb Age Characteristics of Main Rivers around Jianghan Basin and Implications of Provenance Tracing[J].Acta Geoscientia Sinica,2022,43(1):73-81.
Authors:LIN Xu  WU Zhong-hai  ZHAO Xi-tao  ZHANG Yang  CHEN Ji-xin  LIU Hai-jin
Institution:College of Civil Engineering and Architecture, Three Gorges University;Institute of Geomechanics, Chinese Academy of Geological Sciences;Institute of Geology and Geophysics, Chinese Academy of Science; School of Earth Sciences, East China University of Technology
Abstract:Jianghan Basin, located in the north of the Yangtze Plate, is a key area for the study of the evolution of the Yangtze River. Zircon is a common accessory mineral in fluvial sediments, and its U-Pb age spectrum has been widely used in provenance tracing studies. However, it has not been systematically studied in Jianghan Basin. In this study, the U-Pb ages of 922 detrital zircons from 12 inflow rivers in the Jianghan Basin were analyzed using laser denudation inductively coupled plasma mass spectrometry (LA-ICP-MS). A multidimensional discriminant map (MDS) combined with the reported U-Pb ages of detrital zircons from rivers was employed to assess the U-Pb ages of detrital zircons from 12 inflow rivers. Further, the U-Pb age variation of detrital zircons from the main inflow rivers in Jianghan Basin was discussed herein. The U-Pb peak age composition of detrital zircons from the Yangtze River, Juzhang River, and Qingjiang River is different. The U-Pb age of detrital zircons in the Yangtze River and Hanjiang River, the two rivers with the largest sediment transport capacity in the Jianghan Basin, are different. The U-Pb age composition of detrital zircons in the Dabie Mountains is different from that of Hanjiang River and the Yangtze River. The U-Pb age composition of detrital zircons from the Mufu Mountains are different from the Yangtze River and the Xiangjiang River. The U-Pb age composition of detrital zircons from Qingjiang, Lishui and Yuanjiang rivers in the Wuling Mountains are different from Xiangjiang and Zijiang rivers. These differences reflect the influence of regional provenance on the sedimentary material composition of these streams. Therefore, the U-Pb ages of detrital zircons from the surrounding rivers of the Jianghan Basin have a good application prospect in the study of basin-mountain coupling and river evolution in the Jianghan Basin.
Keywords:Jianghan Basin  zircon  U-Pb ages  provenance tracing
本文献已被 维普 万方数据 等数据库收录!
点击此处可从《地球学报》浏览原始摘要信息
点击此处可从《地球学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号