世界地质    2017 36 (3): 806-825   ISSN: 1004-5589  CN: 22-1111/P   小兴安岭北麓高松山金矿床赋矿围岩锆石U-Pb年代学、地球化学、岩石成因及其地质意义 刘阳1, 孙景贵1, 任亮1,5, 韩吉龙1, 王清海2, 古阿雷3, 赵克强4 1. 吉林大学地球科学学院, 长春 130061; 2. 吉林大学东北亚国际地学研究与教学中心, 长春 130026; 3. 中国地质调查局天津地质调查中心, 天津 300170; 4. 中国地质科学院地球物理地球化学勘察研究院, 河北廊坊 065000; 5. 内蒙古农业大学水利与土木建筑工程学院, 呼和浩特 010018 收稿日期 2017-03-08  修回日期 2017-06-20  网络版发布日期 null 参考文献  [1] 章凤奇.松辽盆地北部早白垩世火山事件与地球动力学:博士学位论文[D]. 杭州:浙江大学,2007. ZHANG Feng-qi. Early Cretaceous volcanic event in the northern Songliao Basin and its geodynamics:doctor's degree thesis[D].Hangzhou:Zhejiang University,2007. [2] 许文良,王枫,裴福萍,等. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J]. 岩石学报,2013,29(2):339-353. XU Wen-liang,WANG Feng,PEI Fu-ping,et al. Mesozoic tectonic regimes and regional ore-forming background in NE China:constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J]. Acta Petrologica Sinica,2013,29(2):339-353. [3] 张吉衡. 大兴安岭中生代火山岩年代学及地球化学研究:博士学位论文[D]. 北京:中国地质大学,2009. ZHANG Ji-heng. 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Acta Petrologica Sinica,2008,24(6):1145-1174. 通讯作者: 孙景贵(1961),男,博士,教授,主要从事岩浆、热液矿床的教学与研究工作.E-mail:sunjinggui@jlu.edu.cn