2021年4月10日爪哇南部地震的应力分析及特征

Rahmat Setyo Yuliatmoko, Sulastri Sulastri
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This study uses seismogram data for the earthquake south of East Java on April 10, 2021, with a radius (∆) of 300-1000 recorded at MEEK, MORW, and ARMA stations in Australia. It calculates the amount of stress based on the stress drop, while the stress column determines the stress mechanism. Calculation of stress drop from the source spectrum is obtained by the deconvolution method, namely the seismogram component separation technique in the form of Source (f), Path (f), Site (f), and Instrument (f). The analysis of the observed displacement spectrum used the Nelder Mead Simplex nonlinear inversion method. Meanwhile, the Stress Columb calculation was obtained using the Columb 3.3 program from the United States Geological Survey (USGS). The result of this research is that the stress drop value is 1.69 MPa, with the type of focus mechanism being a thrust fault in the sea. The earthquake in the south of East Java was caused by rock activity in the intraplate. The value of the stress drop is more significant when compared to the subduction contact area. This area is of intraplate rock with various variations, and earthquakes are rare. This study aims to analyze the stress, both the magnitude of the stress drop and the mechanism of the column stress results, so that the stress caused by the earthquake can be known and why the earthquake in the south of East Java is destructive. The quake in Southeast Java is classified as dangerous, not because of the magnitude of the stress generated or its mechanism. The damage was due to the amplification of earthquake waves in the building. The injury occurred because most of the buildings were built on soft soil, especially in several areas in East Java, such as Lumajang, Pasuruan, Trenggalek, Probolinggo, Ponorogo, Jember, Tulunggagung, Nganjuk, Pacitan, and several urban areas, namely Blitar, Kediri, Malang, and Stone. 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引用次数: 0

摘要

2021年4月10日发生在东爪哇南部的地震被列为破坏性地震。这次地震的二次影响相当大。许多房屋倒塌,伤亡人数不少。这次地震的独特之处在于,破坏性地震通常发生在浅层,但6.1级地震被归类为海上中深度地震。东爪哇南部的地震被归类为板块内地震,因为它位于大陆板块上,而不是板块接触区。问题是,对建筑物的破坏是否纯粹是由于地震释放的压力的大小,或者是否有其他因素。本研究使用了澳大利亚MEEK、MORW和ARMA台站记录的2021年4月10日东爪哇以南地震的地震记录资料,地震半径∆为300-1000。它根据应力降计算应力量,而应力柱确定应力机理。通过反褶积方法,即以震源(f)、路径(f)、场地(f)、仪器(f)形式的地震记录分量分离技术,计算震源谱的应力降。对观测位移谱的分析采用Nelder Mead单纯形非线性反演方法。同时,利用美国地质调查局(USGS)的Columb 3.3程序进行应力柱计算。研究结果表明:应力降值为1.69 MPa,震源机制类型为海上逆冲断层。东爪哇南部的地震是由板块内的岩石活动引起的。与俯冲接触面积相比,应力降值更为显著。该地区为板内岩,变化多样,地震较少。本研究旨在分析应力,包括应力下降的大小和柱应力结果的机制,从而了解地震引起的应力以及东爪哇南部地震具有破坏性的原因。爪哇东南部的地震被列为危险级别,不是因为产生的压力大小或其机制。损坏是由于建筑物内地震波的放大造成的。造成伤害的原因是大多数建筑物建在软土上,特别是在东爪哇的几个地区,如Lumajang、Pasuruan、Trenggalek、Probolinggo、Ponorogo、Jember、Tulunggagung、Nganjuk、Pacitan,以及几个城市地区,即Blitar、Kediri、Malang和Stone。因此,有必要减轻地震灾害,特别是在居住在软土上的人口稠密地区。这种减灾努力是根据抗震标准建造建筑物,并避免在有可能扩大地震波的地区开发,从而最大限度地减少伤亡的发生。
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STRESS ANALYSIS AND CHARACTERISTICS DUE TO THE SOUTH JAVA EARTHQUAKE, APRIL 10, 2021
The April 10, 2021, earthquake in the south of East Java was classified as destructive. The secondary impact of this earthquake was quite significant. Many houses collapsed, and not a few casualties. This earthquake is unique because usually, destructive earthquakes occur at shallow depths, but earthquakes with a magnitude of 6.1 are classified as medium-depth earthquakes at sea. The earthquake in the south of East Java is classified as an intraplate earthquake because it is located on the continental plate, not in the plate contact area. The question is whether the damage that occurred to the building was purely due to the magnitude of the stress released by the earthquake or whether there were other factors. This study uses seismogram data for the earthquake south of East Java on April 10, 2021, with a radius (∆) of 300-1000 recorded at MEEK, MORW, and ARMA stations in Australia. It calculates the amount of stress based on the stress drop, while the stress column determines the stress mechanism. Calculation of stress drop from the source spectrum is obtained by the deconvolution method, namely the seismogram component separation technique in the form of Source (f), Path (f), Site (f), and Instrument (f). The analysis of the observed displacement spectrum used the Nelder Mead Simplex nonlinear inversion method. Meanwhile, the Stress Columb calculation was obtained using the Columb 3.3 program from the United States Geological Survey (USGS). The result of this research is that the stress drop value is 1.69 MPa, with the type of focus mechanism being a thrust fault in the sea. The earthquake in the south of East Java was caused by rock activity in the intraplate. The value of the stress drop is more significant when compared to the subduction contact area. This area is of intraplate rock with various variations, and earthquakes are rare. This study aims to analyze the stress, both the magnitude of the stress drop and the mechanism of the column stress results, so that the stress caused by the earthquake can be known and why the earthquake in the south of East Java is destructive. The quake in Southeast Java is classified as dangerous, not because of the magnitude of the stress generated or its mechanism. The damage was due to the amplification of earthquake waves in the building. The injury occurred because most of the buildings were built on soft soil, especially in several areas in East Java, such as Lumajang, Pasuruan, Trenggalek, Probolinggo, Ponorogo, Jember, Tulunggagung, Nganjuk, Pacitan, and several urban areas, namely Blitar, Kediri, Malang, and Stone. So, there is a need for earthquake disaster mitigation, especially in densely populated areas that live on soft soil. This mitigation effort is to minimize the occurrence of casualties by building buildings according to earthquake-resistant standards and avoiding development in the regions that have the potential for amplification of earthquake waves.
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