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Seismic hazard evaluation in Anjar city area of western India: Microtremor array measurement

机译:印度西部安贾尔市地区的地震灾害评估:微震阵列测量

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In western India during the Bhuj earthquake (Mw 7.6) on January 26, 2001, the Anjar City at 30 km southwest of Bhuj experienced three types of damage scenario: severely damaged, less damaged and non-damaged. Similar damage patterns were also observed for the 1819 (Mw 7.8) and the 1956 (Mw 6.0) earthquakes. Microtremor array measurements were conducted in and around the Anjar city to examine the strength of soil structures and damage pattern. Significant differences are observed in frequencies and amplitudes in horizontal-to-vertical spectral ratio (HVSR) using microtremor measurements. The severely-damaged site shows two peak amplitudes: 2.8 at 1.2 Hz; and 4.0 at 8.0 Hz. The less-damaged site also shows two amplitudes: 2.5 and 2.1 at 1.4 Hz; and 2.0 Hz, respectively. The non-damaged site, on the other hand, shows that the HVSR curves become almost flatter. Similar results for three types of damage scenario based on analyses of earthquake records are also observed for the study area. The microtremor array measurements has revealed shear wave velocity V-s >= 400 m/s at 18 m depth in the non-damaged, at 40 m in the less-damaged and at 60 m depth in the severely-damaged sites. The site amplitudes and the Vs values show a good correlation with the soil characteristics and damage pattern, suggesting that strength of soil layers at varying depths is a dictating factor for the estimate of the earthquake risk evaluation of the area under study. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在2001年1月26日的普杰地震(Mw 7.6)期间,印度西部的普杰西南30公里处的安贾尔市遭受了三种破坏:严重破坏,较少破坏和未破坏。在1819(Mw 7.8)和1956(Mw 6.0)地震中也观察到类似的破坏模式。在安贾尔市及其周边地区进行了微震阵列测量,以检查土壤结构的强度和破坏模式。使用微震测量,观察到水平与垂直频谱之比(HVSR)的频率和幅度存在明显差异。严重损坏的位置显示两个峰值幅度:1.2 Hz时为2.8;峰值频率为1。和8.0 Hz时为4.0。损坏较小的位置还显示两个振幅:1.4 Hz时为2.5和2.1;振幅为2.5 Hz。和2.0 Hz。另一方面,未损坏的位置表明HVSR曲线几乎变得平坦。在研究区域,基于地震记录的分析,对三种破坏情景的结果也相似。显微震颤阵列的测量结果表明,在未损坏的深度为18 m处,在未损坏的深度为40 m处以及在严重损坏的位置为60 m处,剪切波速度V-s> = 400 m / s。场地振幅和Vs值与土壤特征和破坏模式显示出良好的相关性,表明不同深度的土壤层强度是估算研究区域地震风险评估的决定性因素。 (C)2015 Elsevier Ltd.保留所有权利。

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