引文
车自成,刘良,刘洪福,罗金海.1998.阿尔金断裂系的组成及相关中新生代含油气盆地的成因特征.中国区域地质,17(4):377—384.Che Zicheng,Liu Liang,Liu Hongfu and Luo Jinhai.1998.The constituents of the Altun fault systemand genetic characteris-tics of related Meso-Cenozoic petroleum-bearing basin.Regional Geology ofChina,17(4):377—384.
陈正乐,万景林,王小凤,陈宣华,潘锦华.2002.阿尔金断裂带8Ma左右的快速走滑及其地质意义.地球学报,23(4):295—300.Chen Zhengle,Wan Jinglin,Wang Xiaofeng,Chen Xuanhua and Pan Jinhua.2002.Rapid strike-slip of the Altyn Tagh faultat8Ma and its geological implications.Acta Geoscientia Sinica,23(4):295—300.
陈正乐,张岳桥,王小凤,陈宣华.2001.新生代阿尔金山脉隆升历史的裂变径迹证据.地球学报,22(5):413—418.Chen Zhengle,Zhang Yueqiao,Wang Xiaofeng and Chen Xuanhua.2001.Fission track dating of apatite constrains on the Ce-nozoic uplift of the Altun Tagh Mountain.Acta Geoscientia Sinica,22(5):413—418.
陈宣华,尹安,Gehrels G E,王小凤,Cowgill E S,Grove M,Harrison TM,陈正乐.2002.青藏高原北缘中生代伸展构造40Ar-39Ar测年和MDD模拟.地球学报,23(4):305—310.Chen Xuanhua,Yin An,Gehrels G E,Wang Xiaofeng,Cowgill E S,Grove M,Harrison TMand Chen Zhengle.2002.Mes-ozoic extension in northern Tibetan Plataeu:40Ar-39Ar analyses and MDD modeling.Acta Geoscientia Sinica,23(4):305—310.
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刘永江,叶慧文,葛肖虹,陈文,刘俊来,任收麦,潘宏勋.2000.阿尔金断裂变形岩激光微区40Ar-39Ar年龄及其构造意义.科学通报,45(19):2101—2104.Liu Yongjiang,Ye Huiwen,Ge Xiaohong,Chen Wen,Liu Junlai,Ren Shoumai and Pan Hongxun.2001.Laser probe40Ar-39Ar dating of mica on the deformed rocks from Altun Fault and its tectonic implications,western China.ChineseSci.Bull.,46(4):322—325.
刘永江,葛肖虹,叶慧文,刘俊来,Neubauer F,Genser J,潘宏勋,任收麦.2001.晚中生代以来阿尔金断裂的走滑模式.地球学报,22(1):23—28.Liu Yongjiang,Ge Xiaohong,Ye Huiwen,Liu Junlai,Neubauer F,Genser J,Pan Hongxun and Ren Shoumai.2001.Strike-slip model for Altun Tagh fault developed since Late Mesozoic.Acta Geoscientia Sinica,22(1):23—28.
刘永江,葛肖虹,Genser J,Neubauer F,Friedl G,常丽华,任收麦,Handler R.2003.阿尔金断裂带构造活动的40Ar-39Ar年龄证据.科学通报,48(12):1335—1341.Liu Yongjiang,Ge Xiaohong,Genser J,Neubauer F,Friedl G,Chang Lihua,Ren Shoumai and Handler R.2003.40Ar-39Arage evidence for Altun fault tectonic activities in western China.Chinese Sci.Bull.,48(18):2024—2030.
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