|
[1] 李坪主编. 1993. 鲜水河—小江断裂带[M]. 北京:地震出版社. 。
[2] 张国民,马宏生,王辉,李丽. 2004. 中国大陆活动地块与强震活动关系[J]. 中国科学D辑,34(7):591~599。
[3] 虢顺民,向宏发,周瑞琦,等. 1999. 滇西南龙陵—澜沧断裂带:中国大陆地壳上一条新生的破裂带[J].
科学通报,44(19):2118~2121。
[4] 柴天俊,杨继武.1992.红河断裂带新构造活动的地质地貌特征[J].云南地质,11(3):260~267。
[5] 张国民,马宏生,王辉,李丽. 2004. 中国大陆活动地块与强震活动关系[J]. 中国科学D辑,34(7):591~599。
[6] 张培震,邓起东,张国民等. 2002. 中国大陆的强震活动与活动地块[J]. 中国科学(D)(33)增刊:12~20。
[7] 王绍晋,龙晓帆. 2004. 用综合段层面解分析红河断裂带的现代构造应力场[J]. 中国大陆地震学与地球内部物理学研究进展(陈运泰,滕吉文,阚荣举,王椿镛主编),地震出版社,767~776。
[8] 计凤桔,虢顺民,向宏发.1997. 红河断裂带第四纪活动的时空演化特征[J].地震地质,
19(2):108~114。
[9] 向宏发,张晚霞,虢顺民,徐锡伟. 1999. 新生破裂带的识别类型划分及其构造意义[J]. 中国地震,15(3):257~267。
[10] Buechfiel B.C.,Wang Erchie. 2003. Northwest~trending,
middle Cenozoic, left~lateral faults in southern Yunnan, Chian[J]. Journal
of Structural Geology, 25:781~792.
[11] Gutenberg B.,Richter C.F. 1954. Seismicity of
the earth and associated phenomena[M]. Princeton University Press, Princeton,
New Jersey. 16~25.
[12 ] Huangfu Gang. 1998. The M=7.0 Lijiang Earthquake
in Yunnan on February 3[J]. Earthquake Prognostics Strategy, EPICenter.
[13] Huangfu Gang, Su Youjin, Shi Shaoxian. 2004. Study
on Seismicity in the Yunnan Region in the 20th Century[J], Vol.27, supp.,p1~11.
[14] Isacks B.L., Oliver J., Sykes
L.R. 1968. Seismology and the new tectonics[J]. J. Geophys. Res., 73:5855~5900.
[15] Kagan, Y. Y. and D. D. Jackson, Long –term earthquake
clustering[J], Geophys. J. Int., vol.104, pp. 117~113, 1991.
[16] Kan R.J., Hu H.X., Zeng R.S., Mooney W.D., McEvilly
T.V. 1986. Crustal structure of Yunnan Province, People’s Republic of
China, from seismic refraction profiles[J]. Science, 234: 433~437.
[17] Kayal J.R. 2001. Microearthquake activity in some
parts of the Himalaya and the tectonic model[J]. Tectonophysics, 339:
331~351.
[18] Kumar S., Mahajan A.K. 2001. Seismotectonics of
the Kangra region, Northwest Himalaya[J]. Tectonophysics, 331:359~371.
[19] Lee Haoyang et. al. 2003. Miocene Jiali faulting
and its implications for Tibetan tectonic evolution[J]. Earth and Planetary
Science Letters,205:185~194.
[20] Leloup P.H., et al,1995,The Ailao Shan—Red River
shear zone (Yunnan,China) tertiary transform boundary of Indochina [J].Tectonophysics,251(4):3~
84.
[21] Molnar P, Tapponnier P. 1975. Cenozoic tctonics
of Asia: Effects of a continental collision[J]. Science, 189: 419~426.
[22] Owens T.J.and Zandt G. 1997. Implications of crustal
property variations for model of Tibetan Plateau evolution[J]. Nature,
387:37~43.
[23] Purnachandra Rao N.,Ravi Kumar M., Tsukuda T.
2003. Current deformation of the Himalaya~Tibet~burma seismic belt: inferences
from seismic activity and strain rate analysis[J]. Journal of Geodynamics,
36:485~496.
[24] Scholz, C. H.,C.A. Aviles and S.G. Wesnousky.
1986. Scaling differences between large interplate and intraplate earthquakes[J].
BSSA, 76(1): 65~70.
[25] Sykes, L. R. and S. P. Nishenko, Probabilities
of occurrence of large plate rupturing earthquakes for the San Andreas,
San Jacinto, and Imperial faults, California, 1983—2003[J], J. G. R.,
vol.89, No.B7, 1984.
[26] Tapponnier P, Xu Zh, Roger E, et al. 2001. Oblique
stepwise rise and growth of the Tibetan Plateau. Science[J], 294: 1671~1677.
[27] Tapponnier P., Molnar P., 1976. Slip~line field
theory and large scale continental tectonics[J]. Nature, 264: 319.
[28] Zeng R.S. 1985. The Mesozoic fold belt between
the Himalayan collision belt and Eurasian plate[J]. EOS, 6S, 46, 1074.
[29] Bhattacharjee C.C. 1991. Tectonophysics, 191:
213~222.
[30] Saikia M.M., Kotoky P., Duarah R. 1987. Tectonophysics,
134: 145~152.
[31] Cheng Wanzheng. 2003. A sequential step-by-step
characteristics of grouped strong earthquakes in Sichuan-Yunnan Region[J].
Journal of Seismological Research, 26(Sup):38~45.
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