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首页> 外文期刊>Journal of Seismology >Ground-motion predictions in Shillong region, northeast India
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Ground-motion predictions in Shillong region, northeast India

机译:印度东北部西隆地区的地面运动预测

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摘要

We deliver ground-motion prediction equations for Shillong region, northeast India, based on a database generated by finite-fault stochastic simulations. An examination of the regional seismic source characteristics is carried out beforehand. Micro/minor earthquakes (M W < 5.0) nucleating at hypocentral depth <21 km in the region recorded at broadband seismic stations are observed to have Brune stress-drop ranging between 2.8 and 99.9 bars. Likewise, macroseismic intensity data for the 1897 Shillong Earthquake that nucleated at a hypocentral depth of ~35 km places the associated stress-drop at 100−200 bars. The apparent variation of the stress-drop parameter with depth is considered with two source zones namely lower-crust and upper-crust. Equations for the lower-crust predict higher ground-motion levels and exhibit affinity to those developed for stable continental region of Eastern North America. The ground-motion levels predicted by the equations for the upper-crust are relatively lower but are still higher compared with those predicted for tectonically active regions, viz., the Himalayas and Western North America.
机译:我们根据有限故障随机模拟生成的数据库,为印度东北部的西隆地区提供地面运动预测方程。预先检查了区域地震源的特征。在宽带地震台站记录的区域中,在次中心深度<21 km处发生的微/小地震(M W <5.0)成核,其Brune应力降范围为2.8至99.9 bar。同样,1897年西隆地震的大地震烈度数据在震中深度约35 km处成核,从而将相关的应力降置于100-200 bar。在两个震源区即下地壳和上地壳中考虑了应力降参数随深度的表观变化。地壳较低的方程预测地面运动水平较高,并且与针对北美东部稳定大陆地区开发的方程具有相似性。由方程式预测的上地壳的地面运动水平相对较低,但与喜马拉雅山和北美西部等构造活动区域的预测水平相比仍然较高。

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