摘要
库姆塔格沙垄东二长花岗岩体由于缺乏同位素年龄依据,其时代厘定一直存在疑问。1∶5万区域地质矿产调查时,对该岩体进行了锆石SHRIMPU-Pb年龄测定,获得了293Ma±6Ma年龄值,表明该岩体形成于晚石炭世。
The age of the east Shalong monzogranite in Kumtag, East Tianshan, Xinjiang, has long been in question because of the lack of isotope age evidence. During 1:50000 regional geological and mineral survey, SHRIMP U-Pb dating was performed on zircons from this intrusion and an age of 293+6 Ma was obtained. This age suggests that this intrusion formed in the Late Carboniferous.
出处
《地质通报》
CAS
CSCD
北大核心
2006年第8期957-959,共3页
Geological Bulletin of China
基金
新疆维吾尔自治区<新疆哈密地区库姆塔格沙垄西南一带1:5万区域地质矿产调查>项目(编号:XJQDZ2003-28)成果。