苏门答腊海沟及其周边地震易发地区的减灾分析

R. Sinaga, I. S. Ronoatmojo
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引用次数: 0

摘要

印度尼西亚位于欧亚板块、环太平洋板块和印度-澳大利亚板块三个活动板块的交界处。苏门答腊构造受印澳板块和东南欧亚板块两个板块的俯冲作用控制。研究区域位于苏门答腊海沟沿线,使用的数据来自美国地质调查局近50年来的数据,深度为0-60 km,使用的方法为最小二乘法。本研究的目的是预测地震的发生,以尽量减少地震造成的损害。闭锁区的回归期值较高,其影响因素是存在地震间隙,由于海山的俯冲作用,施加在该区域的应力将被隔离,从而使其能够承受地震。但有一天,当岩石不再承受应力时,就会引起大强度的地震。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALYSIS OF EARTHQUAKE-PRONE AREAS FOR DISASTER MITIGATION IN THE SUMATRA TRENCH AND SURROUNDINGS
Indonesia is situated at the junction of three active plates: Eurasia, Circum Pacific, and Indo-Australia.. Sumatran tectonics is controlled by the subduction of two plates, namely the Indo-Australian plate and the southeastern Eurasian plate. The research area is along the Sumatra Trench and the data used are from the United States Geological Survey in  the last 50 years, the depth is 0-60 km, and the methodology used is the least squares method. Purpose of this study, to predict the occurrence of earthquakes with the aim of minimizing the impact of damage that occurs in earthquakes. The Locked Area has a high return period value, the influencing factor is the existence of a seismic gap, where the stress applied to this area will be isolated due to seamount subduction, so that it can withstand earthquakes. but one day, when the rock can no longer withstand the stress, it will cause an earthquake with large strength.
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