世界地质    2017 36 (3): 751-762   ISSN: 1004-5589  CN: 22-1111/P   大兴安岭环二库新元古代变质辉长岩的厘定及其地质意义 杜兵盈1, 冯志强2, 刘宇崴1, 张铁安1, 赵明胜3, 赵雨生1, 甄淼1 1. 黑龙江省区域地质调查所, 哈尔滨 150080; 2. 太原理工大学地球科学与工程系, 太原 030024; 3. 沈阳师范大学古生物学院, 沈阳 110034 收稿日期 2016-12-22  修回日期 2017-06-19  网络版发布日期 null 参考文献  [1] Sengör A M C, Natal'in B A,Burtman V S. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J]. Nature, 1993, 364:299-307. [2] Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China:termination of the Central Asian Orogenic Belt[J]. Tectonics, 2003, 22:1069-1089. [3] 邵济安,张履桥,肖庆辉,等. 中生代大兴安岭的隆起:一种可能的陆内造山机制[J]. 岩石学报, 2005, 21(3):789-794. SHAO Ji-an, ZHANG Lü-qiao, XIAO Qing-hui, et al. Rising of Da Hinggan Mts in Mesozoic:a possible mechanism of intracontinental orogeny[J]. Acta Petrologica Sinica, 2005, 21(3):789-794. [4] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. 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