Bassin C, Laske G, Masters G. 2000. The current limits of resolution for surface wave tomography in North America. Eos Trans AGU, 81: F897.
[2]
Cheng J, Xu X W, Gan W J, et al. 2012. Block model and dynamic implication from the earthquake activities and crustal motion in the southeastern margin of Tibetan Plateau. Chinese J. Geophys. (in Chinese), 55(4): 1198-1212, doi:10.6038/j.issn.0001-5733.2012.04.016.
[3]
Cheng W Z, Diao G L, Lü G P, et al. 2003. Focal mechanisms, displacement rate and mode of motion of the Sichuan-Yunnan Block. Seismology and Geology (in Chinese), 25(1): 71-87.
[4]
Cui X F, Xie F R, Zhang H Y. 2006. Recent tectonic stress field zoning in Sichuan-Yunnan region and its dynamic interest. Acta Seismologica Sinica (in Chinese), 28(5): 451-461.
[5]
Gan W J, Zhang P Z, Shen Z K, at el. 2007. Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements. J. Geophys. Res., 112(B8): B08416, doi: 10.1029/2005JB004120.
[6]
Gephart J W, Forsyth D W. 1984. An improved method for determining the regional stress tensor using earthquake focal mechanism data: application to the San Fernando earthquake sequence. J. Geophys. Res., 89(B11): 9305-9320.
[7]
Gephart J W. 1990. Stress and the direction of slip on fault planes. Tectonics, 9(4): 845-858.
[8]
Long F, Zhang Y J, Wen X Z, et al. 2010. Focal mechanism solutions of ML≥4.0 events in the Ms6.1 Panzhihua-Huili earthquake sequence of Aug 30, 2008. Chinese J. Geophys. (in Chinese), 53(12): 2852-2860, doi: 10.3969/j.issn.0001-5733.2010.12.008.
[9]
Luo J, Zhao C P, Zhou L Q. 2014. Characteristics of focal mechanisms and stress field of the Chuan-Dian rhombic block and its adjacent regions. Seismology and Geology (in Chinese), 36(2): 405-421.
[10]
Luo Y, Ni S D, Zeng X F, et al. 2010. A shallow aftershock sequence in the north-eastern end of the Wenchuan earthquake aftershock zone. Science in China (Series D): Earth Science (in Chinese), 53(11): 1655-1664.
[11]
Lü J, Zheng X F, Xiao J, et al. 2013. Rupture characteristics and seismogenic structures of the Ms5.7 and Ms5.6 Yiliang earthquake of Sep. 7, 2012. Chinese J. Geophys. (in Chinese), 56(8): 2645-2654, doi: 10.6038/cjg20130814.
[12]
Shen J, Wang Y P, Ren J W. 2001. The Quaternary right-lateral strike-slipping on the Deqin-Zhongdian-Daju Fault zone in Yunnan, China. // Ma Z J ed. Study on Recent Deformation and Dynamics of the Lithosphere of Qinghai-Xizang Plateau (in Chinese). Beijing: Seismological Press,123-135.
[13]
Tapponnier P, Xu Z Q, Roger F, et al. 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294(5547): 1671-1677. doi: 10.1126/Science.105978.
[14]
Wang Y Z, Wang E N, Shen Z K, et al. 2008. GPS-constrained inversion of present-day slip rates along major faults of the Sichuan-Yunnan region, China. Science in China (Series D): Earth Science (in Chinese), 51(9): 1267-1283.
[15]
Wei S J, Zhan Z, Tan Y, et al. 2012. Locating earthquakes with surface waves and Centroid moment tensor estimation. J. Geophys. Res., 117(B4): B04309, doi: 10.1029/2011JB008501.
[16]
Wessel P, Smith W H F. 1991. Free software helps map and display data. Eos, Transactions American Geophysical Union, 72(41): 441-446.
[17]
Xie F R, Zhu J Z, Liang H Q, et al. 1993. The basic characteristics of recent tectonic stress field in southwest region of China. Acta Seismologica Sinica (in Chinese),15(4): 407-417.
[18]
Xu Y, Herrmann R B, Koper K D. 2010. Source parameters of regional small-to-moderate earthquakes in the Yunnan-Sichuan region of China. Bull. Seis. Soc. Am., 100(5B): 2518-2531.doi: 10.1785/0120090195.
[19]
Zhang P Z. 2013. A review on active tectonics and deep crustal processes of the Western Sichuan region, eastern margin of the Tibetan Plateau. Tectonophysics, 584: 7-22, doi: 10.1016/j.tecto.2012.02.021.
[20]
Zhao L, Luo Y, Liu T Y, et al. 2013. Earthquake focal mechanisms in Yunnan and their inference on the regional stress field. Bull. Seis. Soc. Am., 103(4): 2498-2507.doi: 10.1785/0120120309.
[21]
Zhao L S, Helmberger D V. 1994. Source estimation from broadband regional seismograms. Bull. Seis. Soc. Am., 84(1): 91-104.
[22]
Zheng X F, Ouyang B, Zhang D N, et al. 2009. Technical system construction of Data Backup Center for China Seismograph Network and the data support to researches on the Wenchuan earthquake. Chinese J. Geophys. (in Chinese), 52(5):1412-1417, doi: 10.3969/j.issn.0001-5733.2009.05.031.
[23]
Zheng Y, Ma H S, Lü J, et al. 2009. Source mechanism of strong aftershocks (Ms≥5.6) of the 2008/05/12 Wenchuan earthquake and the implication for seismotectonics. Science in China (Series D): Earth Science (in Chinese), 52(6): 739-753.
[24]
Zhu L P, Helmberger D V. 1996. Advancement in source estimation techniques using broadband regional seismograms. Bull. Seis. Soc. Am., 86(5): 1634-1641.
[25]
Zhu L P, Helmberger D V, Saikia C K, et al. 1997. Regional waveform calibration in the Pamir-Hindu Kush region. J. Geophys. Res., 102(B10): 22799-22813.
[26]
Zhu L P, Rivera L A. 2002. A note on the dynamic and static displacements from a point source in multilayered media. Geophys. J. Int., 148(3): 619-627.
[27]
Zoback M L. 1992. First- and second-order patterns of stress in the lithosphere: The world stress map project. J. Geophys. Res., 97(B8): 11703-11728.
[28]
Shen J, Wang Y P, Ren J W, et al. 2003. Quaternary dextral shearing and crustal movement in southeast Tibetan Plateau. Xinjiang Geology (in Chinese), 21(1): 120-125.
[29]
Shen Z K, Lü J N, Wang M, et al. 2005. Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau. J. Geophys. Res., 110(B11): B11409, doi: 10.1029/2004JB003421.
[30]
Socquet A, Pubellier M. 2005. Cenozoic deformation in western Yunnan (China-Myanmar border). Journal of Asian Earth Science, 24(4): 495-515.
