[1] 邓起东, 张维岐. 海原走滑断裂带及其尾端挤压构造[J]. 地震地质, 1989(1): 1-14. [2] 张培震, 郑德文, 尹功明, 等. 有关青藏高原东北缘晚新生代扩展与隆升的讨论[J]. 第四纪研究, 2006, 26(1): 5-13. [3] 向宏发, 虢顺民, 张秉良, 等. 六盘山东麓地区活动构造研究[J]. 国际地震动态, 1998, (7): 23-26. [4] Burchfiel B C, Zhang P Z, Wang Y P, et al. Geology of the Haiyuan fault zone, Ningxia-Hui Autonomous Region, China, and it’s relation to the evolution of the northeastern margin of the Tibetan Plateau[J]. Tectonics, 1991, 10(6): 1091-1110. [5] Deng Q D, Sung F M, Zhu S L, et al. Active faulting and tectonics of the Ningxia-Hui Autonomous Region, China[J]. J. Geophys. Res., 1984, 89(B6): 4427-4445. [6] Zhang P Z, Shen Z K, Wang M, et al. Continuous deformation of the Tibetan Plateau from global positioning system data[J]. Geology, 2004, 32(9): 809-812. [7] 郝明, 秦姗兰, 李煜航, 等. 青藏高原东北缘近期地壳水平运动研究[J]. 大地测量与地球动力学, 2014, 34(3): 99-103. [8] Hao M, Wang Q L, Shen Z K, et al. Present day crustal vertical movement inferred from precise leveling data in eastern margin of Tibetan Plateau[J]. Tectonophysics, 2014, 632: 281-292. [9] McCaffrey R. 2002. Crustal block rotations and plate coupling[J]. Plate boundary zones, 30: 101-122. [10] Okada Y. Surface Deformaiton due to Shear and Tensile Faults in a Half-Space[J]. Bulletin of the Seismological Society of America.1985, 75(4): 1135-1154. [11] Okada Y. Internal Deformation due to Shear and Tensile Faults in a Half-Space[J]. Bulletin of the Seismological Society of America. 1992, 82(2): 1018-1040. [12] Loveless J P and Meade B J. Partitioning of localized and diffuse deformation in the Tibetan Plateau from joint inversions of geologic and geodetic observations[J]. Earth & Planetary Science Letters, 2011, 303(s1-2): 11-24. [13] 赵红格, 刘池洋, 王峰. 鄂尔多斯盆地西缘的构造分区性探讨[J]. 地学前缘, 2005, (4): 542-542. [14] 赵红格, 刘池洋, 姚亚明, 等. 鄂尔多斯盆地西缘差异抬升的裂变径迹证据[J]. 西北大学学报: 自然科学版, 2007, 37(3): 470-474. [15] 张秉良, 向宏发, 虢顺民, 等. 六盘山东麓断裂断层泥的组构特征及其意义[J]. 地震地质, 2004, 22(1): 47-52. [16] 向宏发, 虢顺民, 张秉良, 等. 六盘山东麓活动逆断裂构造带晚第四纪以来的活动特征[J]. 地震地质, 1998(4): 321-327. [17] Humphreys E and Clayton R W. Adaption of back projection tomography to seismic travel time problems[J]. J. Geophys. Res., 1988, 93(93): 1073-1085. [18] Jiang G Y, Xu X W, Chen G H, et al. Geodetic imaging of potential seismogenic asperities on the Xianshuihe-Anninghe-Zemuhe fault system, southwest China, with a new 3D viscoelastic interseismic coupling model[J]. Journal of Geophysical Research Solid Earth, 2015, 120(3): 1855-1873. [19] 童蔚蔚, 王良书, 米宁, 等. 利用接收函数研究六盘山地区地壳上地幔结构特征[J]. 中国科学, 2007(S1): 193-198. [20] 李英康, 高锐, 米胜信, 等. 青藏高原东北缘六盘山—鄂尔多斯盆地的地壳速度结构特征[J]. 地质论评, 2014, 60(5): 1147-1157. [21] 曾融生, 孙为国. 中国大陆莫霍界面深度图[J]. 地震学报, 1995, (3): 322-327. [22] 葛伟鹏, 王敏, 沈正康, 等. 柴达木—祁连山地块内部震间上地壳块体运动特征与变形模式研究[J]. 地球物理学报, 2013, 56(9): 2994-3010. |