Quantifying the Seismicity Parameters of A New Model of Seismic Source Zone for Aceh and Surrounding Areas

Juellyan Juellyan, B. Setiawan, M. Hasan, T. Saidi
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Abstract

Aceh is justified as one of the Indonesian provinces with a high level of seismicity. This high seismicity certainly has a severe negative impact on various aspects of human life in Aceh and the surrounding areas. Various types of efforts must be carried out to solve and mitigate the problem caused by each earthquake in Aceh and the surrounding areas. One aspect that can be carried out to minimize the hazards of seismic activity is the characterization of the source of the earthquake. This characterization can be used for various purposes for further seismic-related studies, including for studying seismic hazard analysis using the probabilistic seismic hazard analysis (PSHA) method. This research aims to determine the characteristics of the seismic source zones for Aceh and the surrounding areas. Based on the geological setting and seismicity catalog data of Aceh and the surrounding areas, a new model of seismic source zones was developed. This new model proposed for Aceh and the surrounding areas is divided into four zones: shallow background seismic source zones (divided into two source zones), two deep background seismic source zones, two megathrust source zones, and one fault zone, namely the Sumatra fault zone. The results of this study suggest that Zone I and Zone II of shallow background seismic source zones have a-values of 2.36 and 4.7, b-values of 0.545, and Mmax of 7.7 and 6.8. Deep background seismic source zone I has an a-value of 4.43 and a b-value of 0.9 with a maximum magnitude of 7 Mw. Meanwhile, deep background seismic source zone II has an a-value of 3.28 and a b-value of 0.755 with a maximum magnitude of 6.1 Mw. Megathrust seismic source zone I has an a-value of 3.53 and a b-value of 0.691 with a Mmax of 7.7 Mw. Meanwhile, the megathrust seismic source zone II has an a-value of 3.81 and a b-value of 0.702 with a Mmax of 7.1 Mw. Sumatra fault seismic source zone has an a-value of 2.88 and a b-value of 0.615 with a Mmax of 6.7 Mw.
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亚齐及周边地区震源带新模型地震活动性参数的量化
亚齐省是印尼地震活跃度较高的省份之一。这种高地震活动性肯定对亚齐和周边地区人类生活的各个方面产生了严重的负面影响。必须采取各种努力来解决和减轻亚齐及周边地区每次地震造成的问题。为了尽量减少地震活动的危害,可以采取的一个方面是确定震源的特征。这种表征可以用于进一步的地震相关研究的各种目的,包括使用概率地震危害分析(PSHA)方法研究地震危害分析。本研究旨在确定亚齐及周边地区震源带的特征。根据亚齐及周边地区的地质背景和地震活动目录资料,建立了新的震源带模型。该模型将亚齐及周边地区划分为4个带:浅背景震源带(分为2个震源带)、2个深背景震源带、2个特大逆冲震源带和1个断裂带(即苏门答腊断裂带)。研究结果表明,浅背景震源带I区和II区a值分别为2.36和4.7,b值分别为0.545,Mmax值分别为7.7和6.8。深背景震源I区a值为4.43,b值为0.9,最大震级为7 Mw。深背景震源II区a值为3.28,b值为0.755,最大震级为6.1 Mw。大逆冲震源ⅰ带a值为3.53,b值为0.691,Mmax为7.7 Mw。大逆冲震源II区a值为3.81,b值为0.702,Mmax为7.1 Mw。苏门答腊断层震源带a值为2.88,b值为0.615,Mmax为6.7 Mw。
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