%0 Journal Article
%T The Geochronological Relationship between the Shaojiwa Formation and the Xingzi Complex Group inNorthwestern Jiangxi and the Constraints on Zircon SHRIMP U-Pb Age<br>庐山筲箕洼组与星子岩群年代地层关系及SHRIMP锆石U-Pb年龄的制约
%A GAO Lin-zhi
%A HUANG Zhi-zhong
%A DING Xiao-zhong
%A LIU Yan-xue
%A ZHANG Chuan-heng
%A WANG Zi-qiang
%A PANG Jian-feng
%A HAN Kun-ying
%A <br>高林志
%A 黄志忠
%A 丁孝忠
%A 刘燕学
%A 张传恒
%A 王自强
%A 庞健峰
%A 韩坤英
%J 地球学报
%D 2012
%I 
%X Ages of (840±6) Ma (MSWD=1.3), (833±4) Ma (MSWD=1.4) and (831±3) Ma (MSWD =1.47) were obtained for spilite and rhyolite from the Shaojiwa Formation. The Xingzi Complex Group has the age of 206Pb/238U (825±5) Ma (MSWD =0.46). In combination of the SHRIMP U-Pb dating of the spilite and rhyolite of the Shaojiwa Formation in the Jiangnan oregen, the authors have determined for the first time that the Xingzi Complex Group is of Neoproterozoic period and lies below the Shaojiwa Formation. These isotopic data from the Shaojiwa Formation are very important for regional correlation of the strata of the corresponding period and tectonic evolution. The zircon U-Pb ages mentioned above determine that Neoproterozoic strata around the age of 820 Ma are developed in northwestern Jiangxi Province. These data contribute to the stratigraphic subdivision and correlation of the metamorphosed rocks in whole Jiangnan old land and help geologists investigate the geological background and ore-forming conditions of the Jiangnan Orogen.
%K Shaojiwa Formation
%K Xingzi Complex Group
%K zircon SHRIMP dating
%K Jiangnan orogen
%K northeastern Jiangxi<br>筲箕洼组
%K 星子岩群
%K 锆石SHRIMP定年
%K “江南造山带”
%K 赣西北地区
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=4471C9E6A56983956B8B3FB4A03BA0AE&yid=99E9153A83D4CB11&vid=27746BCEEE58E9DC&iid=38B194292C032A66&sid=AF507FDD66D991DA&eid=8ED630AD8C61FAE8&journal_id=1006-3021&journal_name=地球学报&referenced_num=0&reference_num=0