%0 Journal Article
%T A discussion on the age of volcanic rocks in Xiaorequanzi Formation, Queletag, Xinjiang<br>新疆觉罗塔格小热泉子组火山岩的时代探讨
%A XIAO WeiFeng
%A WANG ZongXiu
%A LI HaiLong
%A YAN XiLi
%A <br>肖伟峰
%A 王宗秀
%A 李海龙
%A 鄢犀利
%J 岩石学报
%D 2011
%I 
%X Xiaorequanzi Formation is a unit of volcanic rock among Carboniferous-Permian volcano-sedimentary rocks which are widely exposed in Queletag, East Tianshan, Xinjiang. It has been divided into Early Carboniferous by referring the neigboring Digar Formation which is defined to Middle Carboniferous by fossil age. Different ages have been given on Xiaorequanzi copper mine in the southern part of Queletag. In the northern part, isotopic chronology data is absent where we dated it using SHRIMP. Isotopic chronology evidence shows that the volcanic rocks and dyke at Digar and Ganggou are of 271~275Ma. These ages are consistent with the recent results in adjacent region by other geologists. According to present evidence, Xiaorequanzi Formation ought to be Early Permian and other strata units and their relative age may be renewed.
%K Early Permian
%K Chronology
%K SHRIMP
%K Xiaorequanzi Formation
%K Queletag
%K Xinjiang<br>早二叠世
%K 年代学
%K SHRIMP
%K 小热泉子组
%K 觉罗塔格
%K 新疆
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=3897C9445ED3113A96E2C00038645932&yid=9377ED8094509821&vid=DB817633AA4F79B9&iid=59906B3B2830C2C5&sid=61BFD922379BD8FD&eid=928D51A9D788310B&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=81