[1]Institute of Tibetan Plateau, Chinese Academy of Sciences.The 2006 Annual Reports of Zhufeng Compositive of ITP/CAS[R].2007.[中国科学院青藏高原研究所.中国科学院青藏高原研究所珠峰综合实验站2006年度总结报告[R].2007.]
[2]Zhao L S, Sen M K, Stoffa P, et al. Application of very fast simulated annealing to the determination of the crustal structure beneath Tibet[J].Geophysical Journal International,1996,125:355-370.
[3]Zhou Ying. Waveform inverse for fine crustal structure beneath seismic station[D]. Beijing: Institute of Geophysics, Chinese Academy of Sciences,1999.[周莹.接收台站精细地壳结构的波形反演[D]. 北京: 中国科学院地球物理研究所, 1999.]
[4]Wang Weimin, Yao Zhenxing. A Study on the 3D crustal structure beneath Taiwan by teleseismic transform function method[J].Chinese Journal of Geophysics,2003,46(5):628-632.[王卫民,姚振兴.用转换函数方法研究台湾地区三维深部结构[J]. 地球物理学报, 2003, 46(5)：628-632.]
[5]Gao Xing, Wang Weimin, Yao Zhenxing. Crustal structure of China mainland and its adjacent regions[J].Chinese Journal of Geophysics,2005, 48(3): 591-601.[高星,王卫民,姚振兴.中国及邻近地区地壳结构[J].地球物理学报,2005,48(3):591-601.]
[6]Zhu Jieshou, Cao Jiamin, Cai Xuelin,et al.Study for three-dimensional structure of earth interior and geodynamics in China and adjacent land and sea regions[J].Advances in Earth Science, 2003, 18(4):497-503.[朱介寿,曹家敏,蔡学林，等.中国及邻近陆域海域地球内部三维结构及动力学研究[J].地球科学进展, 2003,18(4):497-503.]
[7]Liu Qiyuan, Kind R, Li Shuncheng. The receiver functions at the stations of the Chinese digital seismic network (CDSN) and their nonlinear inversion[J].Chinese Journal of Geophysics,1997, 40(3): 356-367.[刘启元, Kind R,李顺成.中国数字地震台网的接收函数及其非线性反演[J].地球物理学报, 1997,40(3):356-367.]
[8]Wang Erqi, Wang Gang, Fan Chun,et al.Orogeny and gravitational collapse along the convergent plate boundary and their mechanical origin: A case study on the Yarlung Tsangpo-Himalaya Belt[J].Earth Science Frontiers,2006,13(4):18-26. [王二七,王刚,樊春,等.板块汇聚带的造山和重力垮塌作用及其力学成因:以雅鲁藏布江—喜马拉雅山汇聚带为例[J].地学前缘 , 2006,13(4):18-26.]
[9]Liu Yan, Siebel Wolfgang,Li Jian,et al.Characteristics of the main central thrust and southern Tibetan detachment in the Tingri area, southern Tibet, and ages of their activities[J].Geological Bulletin of China,2004,23(7):636-644. [刘焰, Siebel Wolfgang,李剑,等.藏南定日地区主中央冲断层与藏南拆离系的特征及其活动时代[J].地质通报, 2004,23(7):636-644.]
[10]Wang Yang,Zhang Kaijun. Cenozoic polyphase deformation of Tibetan-Himalayan orogen: A review[J].Journal of Nanjing University(natural sciences),2006, 42(2):199-219. [汪洋,张开均.青藏高原新生代构造研究最新进展和构造发展的阶段性[J].南京大学学报:自然科学版, 2006,42(2):199-219.]
[11]Yin An. Cenozoic tectonic evolution of the Himalayan Orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation[J].Earth Science Frontiers,2006, 13(5):416-515. [尹安.喜马拉雅造山带新生代构造演化:沿走向变化的构造几何形态、剥露历史和前陆沉积的约束[J].地学前缘,2006,13(5):416-515.]
[12]Liu Xianbin, Gao Lianfeng, Wan Xiaoqiao,et al. Sequence stratigraphy of the boundary between the Jurassic and the Cretaceous strata in the northern Tethys-Himalayas sea area[J].Journal of Mineralogy and Petrology,2006,26(4):62-68.[刘宪斌,高莲凤,万晓樵,等.特提斯—喜马拉雅北带侏罗纪—白垩纪界线层序地层分析[J].矿物岩石,2006 ,26(4):62-68.]
[13]Wang Erqi, Zhou Yong, Chen Zhiliang,et al.Geologic and geomorphic origin of the East Himalayan Gap[J].Chinese Journal of Ggeology,2001,36(1):122-128.[王二七,周勇,陈智樑,等.东喜马拉雅缺口的地质与地貌成因[J].地质科学,2001,36(1): 122-128.]
[14]Ding Lin. Paleocene deep-water sediments and radiolarian faunas: Implications for evolution of Yarlung-Zangbo foreland basin, southern Tibet[J].Science in China(Series D),2003,33(1):47-58.[丁林.西藏雅鲁藏布江缝合带古新世深水沉积和放射虫动物群的发现及对前陆盆地演化的制约[J].中国科学：D辑, 2003, 33(1): 47-58.]
[15]Zeng Rongsheng, Ding Zhifeng, Wu Qingju,et al.Seismological evidences for the multiple incomplete crustal subductions in Himalaya and southern Tibet[J].Chinese Journal of Geophysics,2000,43(6):780-797.[曾融生,丁志峰,吴庆举,等.喜马拉雅及南藏的地壳俯冲带—地震学证据[J].地球物理学报, 2000,43(6):780-797.]