Quite a large amount of teleseismic profiling has been conducted in the past 10 years or so in the Tibetan Plateau to study the lower crust upper mantle structure, yielding informative data for the geomechanic features ranging from the in depth seismic velocity image, upper mantle anisotropy and the identification of the low velocity body and layer. Along with the improvement in seismic equipment, the method has become the major means in the studies on deep seated structures in an inexpensive manner. Marked achievement has been gained in seismic tomography, the study of receiver functions and the analysis in shear wave splitting. However, room for further studies remains.
钱辉, 姜枚, 宿和平, 董英君. 中国天然地震探测深部构造的研究现状与发展[J]. 物探与化探, 2000, 24(1): 1-6,11.
Qian Hui, Jiang Mei, Su Heping, Dong Yingjun . CURRENT STATE AND DEVELOPING TREND OF THE TELESEISMIC STUDY ON DEEP SEATED STRUCTURES IN CHINA. Geophysical and Geochemical Exploration, 2000, 24(1): 1-6,11.
［1］ 姜枚,吕庆田,薛光琦.青藏高原中段天然地震探测地壳和上地幔结构的研究.地球物理学报,1996,39（4）:470～482
［2］ 曾融生,吴大明,Owens T J.中美合作课题“青藏高原地壳上地幔结构及地球动力学的研究”介绍.地震学报,1992,14（增刊）:521～522
［3］ 宿和平,姜枚.天然地震探测地壳上地幔结构的方法与进展.国外地质勘探技术,1995(1):1～4
［4］ 董英君,姜枚,宿和平.宽频地震观测在研究青藏高原深部构造中的前景.中国地质,1997(9):26～28
［5］ 许志琴,姜枚.青藏高原北部隆升的深部构造物理作用.地质学报,1996,70(3):195～206
［6］ 曾融生,丁志峰,吴庆举.喜玛拉雅—祁连山地壳结构与大陆—大陆碰撞过程.地球物理学报,1998,41（1）:49～60
［7］ 曾融生,朱介寿,周兵,等.青藏高原及其东部邻区的三维地震波速度结构与大陆碰撞模型.地震学报,1992,14:523～533
［8］ 姜枚,薛光琦,Wittlinger G,等.青海茫崖—新疆若羌地震探测剖面及其深部构造研究．地质学报,1999,73（2）:153～161
［9］ Wittlinger G,Tapponnier P,Poupinet G,et al. Tomographic evidence for localized lithospheric shear along the Altyn Tagh fault.Science,1998,282:74～76
［10］ 丁志峰,曾融生.青藏高原横波分裂的观测研究.地球物理学报,1996,39(2):211～219。
［11］ 史大年,董英君,姜枚,等.西藏定日—青海格尔木剪切波各向异性研究.地质学报,1996,71(4):144～151
［12］ 曾融生,孙为国.青藏高原及其邻区的地震活动性和震源机制以及高原物质东流的讨论.地震学报,1992,14:534～563
［13］ 张春贺,姜枚,史大年,等.阿尔金断裂带地震的定位及其分布特征.地震地磁观测与研究,1998,19（1）
［14］ Bourjot L,Romanowica B.Crust and upper mantle tomography in Tibet using surface waves.Geophys Res Lett ,1992,19(5):881～884
［15］ Savage M K.Seismic anisotropy and mantle deformation:what have we learned from shear wave splitting.Reviews of Geophysics,1999,37(1):65～107
［16］ Jiang M,Hirn A,Poupinet G.Tibetan Plateau seismic experiment:Design and preliminary results.Global Tect & Mettallogeny,1995(4):199～201
［17］ Tapponnier P,Meyer B,Avouac J P,et al. Active thrusting and folding in the Qilian Shan and decoupling between upper crust and mantle in northeastern Tibet. Earth Planet Sci Lett,1990,97:382～403
［18］ Wittlinger G,Masson F,Poupinet G,et al. Seismic tomography of northern Tibet and Kunlun: evidence for crustal blocks and mantle velocity contrasts.EPSL,1996,139:263～279
［19］ 薛光琦,姜枚,史大年,等.利用接收函数探讨阿尔金地区深部构造.地质评论,1999,47（2）
［20］ Kosarev G L,Petersen N V,Vinnik L P.Receiver functions for the Tien Shan analog broadband network:Contrasts in the evolution of structures across the Talasso-Fergana Fault. Journ Geophys Res,1993,98(B3):4437～4448
［21］ Silver P G,Chan W W.Implications for continental structure and evolution from seismic anisotropy.Nature,1988,335:34～39
［22］ Matte Ph,Tapponnier P,Arnaud N,et al.Tectonics of western tibet between the tarim and the indus. Earth Planet Sci Lett,1996,142:311～330
［23］ McNamara D E,Owens T J,Silver P G,Wu F T.Shear wave anisotropy beneath the Tibetan Plateau.Journ Geophys Res,1994,99(B7):13655～13665
［24］ Thurber C H.Local earthquake tomography: velocities and Vp/Vs-theory,in seimic tomography.Iyer H M,Hirahara K ed.Theory and practice.London:Chapman and Hall,1993,563～583
［25］ Hirn A,Jiang M,Sapin M,et al.Seismic anisotropy as an indicator of mantle flow beneath the Himalayas and Tibet.Nature,1995,375:571～574
