世界地质    2018 37 (3): 688-701   ISSN: 1004-5589  CN: 22-1111/P   大兴安岭北段裸河组物源及其构造环境：来自地球化学和碎屑锆石年代学的证据 蒋立伟1, 刘永江1,2,3, 冯志强4, 汤超5 1. 吉林大学 地球科学学院, 长春 130061; 2. 中国海洋大学 海洋地球科学学院, 山东 青岛 266100; 3. 海底科学与探测技术教育部重点实验室, 山东 青岛 266100; 4. 太原理工大学 地球科学与工程系, 太原 030009; 5. 中国地质调查局天津地质调查中心 非化石能源矿产实验室, 天津 300170 收稿日期 2017-12-19  修回日期 2018-03-15  网络版发布日期 null 参考文献  [1] 肖文交,舒良树, 高俊,等. 中亚造山带大陆动力学过程与成矿作用[J].新疆地质,2008, 26(1):4-8. XIAO Wen-jiao,SHU Liang-shu, GAO Jun, et al. Continental dynamics of the central Asian orogenic belt and its metallogeny[J]. Xinjiang Geology, 2008, 26(1):4-8. [2] 黄汲清, 姜春发. 从多旋回构造运动观点初步探讨地壳发展规律[J]. 地质学报, 1962, 42(2):3-50. HUANG Ji-qing, JIANG Chun-fa. Preliminary investigation on the evolution of the Earth's crust from the point of view of polycyclic tectonic movements[J].Acta Geologica Sinica, 1962, 42(2):3-50. [3] Tang K D. Tectonic development of Paleozoic foldbelts at the north margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2):249-260. 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