%0 Journal Article
%T Isotopic Age of Shijuli Gabbro in North Qilian Mountain and Its Geological Significance<br>北祁连山石居里辉长岩的同位素年龄及其地质意义
%A SONG Zhong-bao
%A LI Wen-yuan
%A LI Huai-min
%A LI Hui-min
%A LI Ya-zhi
%A LI Chang-an
%A ZHANG Jiang-hu
%A WANG Wei
%A LI Li
%A CHEN Bo
%A <br>宋忠宝
%A 李文渊
%A 李怀坤
%A 李惠民
%A 栗亚芝
%A 李长安
%A 张江华
%A 王伟
%A 李丽
%A 陈博
%J 地球学报
%D 2007
%I 
%X The U-Pb isotopic age of Shijuli gabbro in North Qilian Mountain is (457.9±1.2) Ma. The Shijuli gabbro is located in the south of the Shijuli copper deposit and is obviously related to this deposit. Although the metallogenic age of this deposit is not known, studies show that it was formed in Caledonian, with the rock-forming age earlier than the ore-forming age. This possibly suggests that the rock body provided heat for the deposit. As this area has many intermediate-acid rocks, the determination of the rock-forming age has an important theoretical and practical significance in search for the Cyprus massive sulfide ore deposits in this area.
%K Shijuli gold deposit
%K gabbro
%K rock-forming age
%K ore-forming age
%K north Qilian mountains<br>石居里铜矿
%K 辉长岩
%K 成岩时代
%K 成矿时代
%K 北祁连山
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=82E53A58B96F5AABB3B7D19085BBB415&yid=A732AF04DDA03BB3&vid=D3E34374A0D77D7F&iid=CA4FD0336C81A37A&sid=DF92D298D3FF1E6E&eid=F3090AE9B60B7ED1&journal_id=1006-3021&journal_name=地球学报&referenced_num=1&reference_num=0