Coseismic and postseismic deformation from the 2007 Bengkulu earthquake based on GPS Data

IF 0.1 Q4 GEOSCIENCES, MULTIDISCIPLINARY Riset Geologi dan Pertambangan Pub Date : 2021-12-30 DOI:10.14203/risetgeotam2021.v31.1182
I. Meilano, S. Susilo, E. Gunawan, S. Rahmadani
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Abstract

On September 12, 2007, a M8.5 megathrust earthquake occurred along the Sunda trench near Bengkulu, West Sumatra. GPS data in Sumatra have indicated the coseismic and postseismic deformations resulting from this earthquake. Our estimate of coseismic displacements suggests that the earthquake displaced up to ~1.8m at GPS stations located north of the epicenter. Moreover, our principal strain estimation in the region suggests that the maximum coseismic extensional strain is ~40 ppm. Our analysis of GPS data in the region suggests that the postseismic decay of the 2007 Bengkulu earthquake was 46 days, estimated using a logarithmic function.
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基于GPS数据的2007年蚌库鲁地震同震和震后形变
2007年9月12日,西苏门答腊岛明库鲁附近的巽他海沟发生了8.5级的大型逆冲地震。苏门答腊岛的GPS数据显示了这次地震造成的同震和震后形变。我们对同震位移的估计表明,在震中以北的GPS站点,地震位移高达1.8米。此外,我们在该地区的主应变估计表明,最大同震伸展应变为~40 ppm。我们对该地区GPS数据的分析表明,2007年明库鲁地震的震后衰减是46天,使用对数函数估计。
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来源期刊
Riset Geologi dan Pertambangan
Riset Geologi dan Pertambangan GEOSCIENCES, MULTIDISCIPLINARY-
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