地质通报2013，Vol.32Issue(7)：996-1005,10.
江山-绍兴断裂带铁沙街组变流纹岩SHRIMP锆石U-Pb测年及其意义
Geochronographic dating of the Tieshajie Formation in the Jiangshan-Shaoxing fault zone and its implications
摘要
Abstract
This paper will report some SHRIMP U-Pb ages (1132Ma±8Ma,1140Ma±7Ma,1143Ma±9Ma and 1172Ma±10Ma) of meta-rhyolite of the Tieshajie Formation in the Jiao-Shao fault zone,which belongs to the Northern margin of Cathaysia.Combine of those dating,we will try to discuss the tectonic set of the Tianli schist,Zhoutan Complex and Wanyuan Complex.According to the isotopic dating,it is important for limit the strata correlation and tectonic evolution in the Jiao-Shao fault zone.The dating above mentioned shows the depositional strata of an ace-basin system in 1.1Ga,which is represented inner ace between the Yangtze and Cathayasia and the Huaiyu area is an extensional basin of the back-are.The chronostratigraphic dating of the Tieshajie Formation proved the reliable isotopic evidence for the correlation of the metamorphosed strata in the Jiang-Shao fault zone.关键词
江绍断裂带/铁沙街组/SHRIMP锆石U-Pb年龄/江西Key words
Jiang-Shao fault zone/ Tieshajie Formation/ SHRIMP zircon U-Pb daring/ Jiangxi Province分类
天文与地球科学引用本文复制引用
高林志,刘燕学,丁孝忠,宋志瑞,黄志忠,张传恒,张恒,史志刚..江山-绍兴断裂带铁沙街组变流纹岩SHRIMP锆石U-Pb测年及其意义[J].地质通报,2013,32(7):996-1005,10.基金项目
中国地质调查局项目(编号:12120113013900)和科技基础性工作专项项目(编号:2011FY120100) （编号:12120113013900）
