HUANG FUMING, YANG ZHIXIAN. 1987: STRESS ACCUMULATION AND RELEASE IN THE XIANSHUIHE FAULT ZONE. Acta Seismologica Sinica, 9(2): 128-142.
Citation: HUANG FUMING, YANG ZHIXIAN. 1987: STRESS ACCUMULATION AND RELEASE IN THE XIANSHUIHE FAULT ZONE. Acta Seismologica Sinica, 9(2): 128-142.

STRESS ACCUMULATION AND RELEASE IN THE XIANSHUIHE FAULT ZONE

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  • Published Date: September 01, 2011
  • In this paper, on the basis of historical data of earthquakes with magnitudes M6, the seismicity in the Xianshuihe fault zone has been studied, and the stress accumulation and release in the fault zone has been further studied by using dislocation model of the fault. The results show that in Daofu, the activity of strong earthquakes along the fault is divided into two active segments: the northwestern and southeastern segments. Strong earthquakes occurred alternately on these active segments. The seismic energy release seems to be quasi-periodic, and the average recurrence period of earthquakes with magnitude M7 is 27.6 years. This paper has shown the patterns of stress release due to the strong earthquakes occurring in three different time spans (1700-1811, 1816-1967, 1816-1982), and has discussed the effect of the stress fields due to the strong earthquakes in the former two time intervals on the occurrence of the first large earthquake that follows. The stress accumulation in the southeastern segment of the fault since 1893 has been calculated, and the corresponding contours of maximum shear stress and hydrostatic stress are shown. Finally, according to the stress accumulation, the additional stress changes and the seismicity as well as the characteristics of strain release curves, we have estimated the seismic trend, and believe that a coming earthquake with magnitude 7.1 to 7.7 may occur in (1) the segment between Kangding and Moxi or (2) the segment between Daofu and Qianning or (3) the segment between Qianning and Kangding in the Xianshuihe fault by the end of this century.
  • 慧、陈天长、蒲晓红、刘万琴、彭美宣和张卫平,鲜水河断裂带强震的破裂过程与地震活动,地震学报,8,1——20,1986, 成尔林、庞明虎,康定——炉霍带的地震活动性及震源机制,地震科学研究,1983,2: 7——14, 钱洪,鲜水河断裂带地震趋势的地质估计,地震研究,3, 165——171,1980, 黄福明、王廷锰,多段断层均匀滑动的应力分布特征,地球物理学报,26〔增刊),678——693,1983, 黄福明,王廷楹,倾斜断层错动产生的应力场,地震学报,2, 1——2 0, I 980, 韩渭宾、黄圣睦,四川鲜水河断裂带七——个地震活动空区,地震学报,5,280——285,1983, Brune, J. N., Seismic moment, Seismicity and rate of o lip along major fault zones, J. Geophys. Res.,73, 777——784, 1968. 刘本培、李建中,鲜水河断裂的活动特征,地震科学研究,1981,3: 30——37, 国家地震局,中国地震烈度区划工作报告,地震出版社,1981, Rodgets, D. A. and M. A. Chinnery, Stress accumulation in the "Iran,ver:e ranges, Southern Califotnia,in: Proc. Conf. on tectonic problems of the San Andreas fault system, 70——79, 1973.

    慧、陈天长、蒲晓红、刘万琴、彭美宣和张卫平,鲜水河断裂带强震的破裂过程与地震活动,地震学报,8,1——20,1986, 成尔林、庞明虎,康定——炉霍带的地震活动性及震源机制,地震科学研究,1983,2: 7——14, 钱洪,鲜水河断裂带地震趋势的地质估计,地震研究,3, 165——171,1980, 黄福明、王廷锰,多段断层均匀滑动的应力分布特征,地球物理学报,26〔增刊),678——693,1983, 黄福明,王廷楹,倾斜断层错动产生的应力场,地震学报,2, 1——2 0, I 980, 韩渭宾、黄圣睦,四川鲜水河断裂带七——个地震活动空区,地震学报,5,280——285,1983, Brune, J. N., Seismic moment, Seismicity and rate of o lip along major fault zones, J. Geophys. Res.,73, 777——784, 1968. 刘本培、李建中,鲜水河断裂的活动特征,地震科学研究,1981,3: 30——37, 国家地震局,中国地震烈度区划工作报告,地震出版社,1981, Rodgets, D. A. and M. A. Chinnery, Stress accumulation in the "Iran,ver:e ranges, Southern Califotnia,in: Proc. Conf. on tectonic problems of the San Andreas fault system, 70——79, 1973.

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