锡巴亚克火山上亚齐地震库仑应力变化分析

Goldberd Harmuda Duva Sinaga, Agoez Loeqman, Ruben Cornelius Siagian, Mardame Pangihutan Sinaga
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引用次数: 0

摘要

从地质条件看,印度尼西亚位于印澳板块、欧亚板块和太平洋板块之间,构造地震多发。然而,自2004年12月26日发生亚齐大地震以来,苏门答腊岛的地质条件发生了重大变化,主要表现为苏门答腊岛西部到南部地区,特别是西巴亚克火山的紧张状况。本研究使用了BMKG和Global CMT的数据,包括震级(Mw)、深度、地震坐标(经纬度)、地震类型、走向、倾角和rake。利用库仑3.3进行分析,得出2015年Sibayak火山库仑应力值最高,库仑应力平均变化0.235 bar,剪切变化0.1909 bar,正向变化0.1106 bar。然而,库仑应力值最低发生在2021年,库仑应力变化适中,为0.0593 bar,剪切为0.0251,正常为0.0849 bar。
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 Coulomb Stress Changes in Aceh Earthquake on Sibayak Volcano
Based on geological conditions, Indonesia is located between the Indo-Australian plate, the Eurasian plate, and the Pacific plate, making Indonesia prone to tectonic earthquakes. However, since the big earthquake that occurred in Aceh on December 26, 2004, the geological conditions in Sumatra have undergone significant changes marked by stressful situations in the western to southern regions of Sumatra, especially on Sibayak Volcano. This study used data from BMKG and Global CMT, which included magnitude (Mw), depth, earthquake coordinates (longitude and latitude), type of earthquake, strike, dip, and rake. From the analysis using Coulomb 3.3, the highest coulomb stress value of Sibayak Volcano was obtained in 2015 with an average change in coulomb stress of 0.235 bar, shear 0.1909 bar, normal 0.1106 bar. However, the lowest coulomb stress value occurs in 2021 with a moderate shift in coulomb stress of 0.0593 bar, shear 0.0251, normal 0.0849 bar.
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