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EARTHQUAKE HAZARD MITIGATION IN CENTRAL AMERICA BY STUDIES OF SEISMIC SOURCE AND GROUND ACCELERATION

机译:地震源和地面加速研究中美洲地震危害缓解

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Central America is a region that has been prone to numerous destructive earthquakes, like the 1972 Managua earthquake, the 1976 Guatemala earthquake and the 1986 San Salvador earthquake among others. Thus, observations of complex faulting of Central American earthquakes have inspired us to investigate rupture processes of earthquakes in that region. E.g., the earthquakes, September 02, 1992, Mw=7. 6, Nicaragua, and the October 18, 1992, Mw=7.1, Colombia, events are notable examples. Thus we are studying source processess of major Central American earthquakes that have occurred during the time of the digital worldwide networks. In order to obtain rupture information we use data from both teleseismic as well as local/regional distances. The techniques we use at telsesimic distances include modelling of the source-time function by inversion of body waves as well as using a empiricial Green's function approach. From the obtained source time function of the 1992 Colombia earthquake we find that on one third of the fault the slip is 70% larger than the average.
机译:中美洲是一个易于众多破坏性地震的地区,如1972年的马那亚地震,1976年危地马拉地震和1986年的圣萨尔瓦多地震等。因此,中美洲地震复杂断层的观察激发了我们调查该地区地震的破裂过程。例如,地震,1992年9月02日,MW = 7。 6,尼加拉瓜和1992年10月18日,MW = 7.1,哥伦比亚,事件是值得注意的例子。因此,我们正在研究在数字全球网络时发生的主要中美洲地震的源码。为了获得破裂信息,我们使用来自Telesmicic以及局部/区域距离的数据。我们在巨晶距离时使用的技术包括通过体波的反转来建模源时间函数以及使用实际绿色的功能方法。从1992年哥伦比亚地震的所获得的源时间函数,我们发现,在缺口的三分之一上,滑动比平均值大70%。

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