世界地质    2017 36 (3): 862-870,879   ISSN: 1004-5589  CN: 22-1111/P   柴北缘鱼卡地区中侏罗统石门沟组页岩段稀土元素地球化学特征与地质意义 王克兵1,2,3, 孟庆涛1,2,3, 刘招君1,2,3, 孙平昌1,2,3, 徐银波4, 白悦悦1,2,3 1. 吉林大学地球科学学院, 长春 130061; 2. 吉林省油页岩及共生能源矿产重点实验室, 长春 130061; 3. 油页岩与共生能源矿产成矿及勘查开发重点实验室, 长春 130061; 4. 中国地质调查局油气资源调查中心, 北京 100029 收稿日期 2016-10-26  修回日期 2016-11-28  网络版发布日期 null 参考文献  [1] 孟庆涛,刘招君,胡菲,等. 桦甸盆地始新统油页岩稀土元素地球化学特征及其地质意义[J]. 吉林大学学报:地球科学版,2013,34(2):390-399. MENG Qin-tao,LIU Zhao-jun, HU Fei,et al. Geochemical charateristics of Eocene oil shale and its geological significance in Huadian Basin[J]. Journal of Jilin University:Earth Science Edition,2013,34(2):390-399. [2] Nesbitt H W. Mobility and fractionation of rare earth elements during weathering of a granodiorite[J]. Nature,1979,279:206-210. [3] 邓硕,刘招君,孙平昌,等. 松辽盆地东南隆起区上白垩统嫩江组泥页岩段地球化学特征与物源分析[J]. 世界地质,2016,35(1):108-122. DENG Shuo,LIU Zhao-jun,SUN Ping-chang,et al. 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