世界地质    2018 37 (3): 737-746,760   ISSN: 1004-5589  CN: 22-1111/P   内蒙古荷尔勿苏铅锌矿区二叠纪侵入岩成因：锆石U-Pb年代学与岩石地球化学制约 王春光1, 孙国胜2, 孙九达2, 牛军平1, 张锐1, 王子维1, 夏磊1 1. 吉林省地质勘查基金管理中心, 长春 130061; 2. 吉林大学 地球科学学院, 长春 130061 收稿日期 2018-01-30  修回日期 2018-06-20  网络版发布日期 null 参考文献  [1] 曾庆栋, 刘建明, 张作伦,等. 华北克拉通北缘鸡冠山斑岩钼矿床成矿年代及印支期成矿事件[J]. 岩石学报, 2009, 25(2):393-398. ZENG Qing-dong, LIU Jian-ming, ZHANG Zuo-lun, et al. Ore-forming time of the Jiguanshan porphyry molybdenum deposit, northern margin of North China Craton and the Indosinian mineralization[J]. Acta Petrologica Sinica, 2009, 25(2):393-398. [2] 赵一鸣, 张德全. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M].北京:地震出版社, 1997:1-161. ZHAO Yi-ming, ZHANG De-quan. Metallogeny and prospective evaluation of copper-polymetallic deposits in the Da Hinggan Mountains and its adjacent regions[M]. Beijing:Seismological Press, 1997:1-161. [3] 张振法, 葛昌宝, 常忠跃. 中华地台与兴蒙古生代地槽褶皱区界线的重新厘定[J]. 物探与化探, 2002,26(2):83-96. ZHANG Zhen-fa, GE Chang-bao, CHANG Zhong-yue. 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The SHRIMP zircon U-Pb dating and geochemical features of Bairendaba diorite in the Xilinhaote area, Inner Mongolia, China[J]. Geological Bulletin of China, 2010, 29(5):688-696. 通讯作者: 孙国胜(1964),男,副教授,主要从事矿床地球化学的教学和研究.E-mail:sgsh8888@163.com