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A Seismic Intensity Survey of the 1 April 2014 M 8.2 Iquique, Chile, Earthquake and Tsunami, and a Comparison with Strong-Motion Data

机译:2014年4月1日的地震强度调查,2014年4月1日,智利,地震和海啸,以及与强运动数据的比较

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We conducted a regional seismic intensity survey in northern Chile following the 1 April 2014 M 8.2 Iquique earthquake to document the level of damage caused by the earthquake and tsunami. We observed very limited damage at the 204 sites surveyed. The modified Mercalli intensities (MMIs) reached a maximum value of VI adjacent to the earthquake rupture plane. The contours of our MMI map are similar in shape to the contour maps of peak ground acceleration (PGA) and peak ground velocity (PGV). A comparison of our seismic intensities with the recorded PGA and PGV values reveals that our MMI values are one to two units lower than predicted by ground-motion intensity conversion equations (GMICEs). We propose that this is due to the well-engineered buildings and moderate levels of high-frequency (0.5-5 Hz) ground shaking experienced during this earthquake. Whether existing GMICEs consistently overpredict seismic intensities for large sub-duction-zone earthquakes deserves further study.
机译:我们在2014年4月1日智利北部进行了一项区域地震强度调查,据Iquique地震,记录了地震和海啸造成的损害水平。 我们在调查的204个站点观察到损坏非常有限。 修改的梅尔提强度(MMIS)达到了与地震破裂平面相邻的VI的最大值。 我们的MMI地图的轮廓形状类似于峰接地加速度(PGA)和峰值接地速度(PGV)的轮廓图。 我们与记录的PGA和PGV值的地震强度的比较表明,我们的MMI值是一个到两个单位低于地面运动强度转换方程(Gmite)的预测。 我们建议这是由于这种地震期间经验丰富地建造的建筑物和中等水平的高频(0.5-5 Hz)地面震动。 现有的Gmices是否始终如一地覆盖大型海拔地区地震的地震强度值得进一步研究。

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