Geophysics And Geomorphic Observation For Near-Surface Structures Mapping Of Seulimeum Fault On Lamtamot Area, Northern Sumatra

Q3 Earth and Planetary Sciences
M. Yanis, Gozian Islami, N. Ismail
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引用次数: 5

Abstract

In the northern part of Sumatra Island, Indonesia, the Great Sumatran Fault, which can cause an earthquake, was divided into two segments: the Aceh and Seulimeum. An effort to reduce the risk is mapping the fault area, especially in the region that does not clearly show the sign on the surface, e.g., in the Lamtamot area, Indonesia. Electrical resistivity is widely used to study shallow structures, but the method requires more time when applied in a large area. This research explores the potential of an extremely low frequency (very low frequency-electromagnetic; VLF-EM) method to investigate the shallow fault of the Seulimeum segment. Here, the VLF-EM is compared with other geophysical methods such as resistivity and magnetic methods. For comprehensive results, the geomorphic observation that was conducted covered outcrops of the fault and trenching sites in the geophysical study for validating the model. A similar pattern of the VLF-EM and electrical resistivity data has been shown in a two-dimensional profile using data processing. The fault structure can be mapped at a distance of 20–24 m from the profile measurement, which is demonstrated by the low current density associated with the conductive zone from the VLF-EM, and low resistive anomaly in electrical resistivity. The fault can also be confirmed via magnetic intensity, which significantly increases at the same distance (20–25 m) of the VLF-EM and electrical resistivity. The geomorphic observation shows outcrops of fault activity, such as fault scarp, fractures, and faults, in the same direction as the Seulimeum segment, while scrap extends in the northwest direction up to ~20 m around the geophysical surveys. As revealed by the results, the VLF-EM method combined with other geophysical surveys and geomorphic observation can be used as a technique to image the fault that shows the shallow structure of the Seulimeum fault at 20–32 m along the profile.
北苏门答腊Lamtamot地区Seulimeum断裂带近地表构造填图的地球物理与地貌观测
在印度尼西亚苏门答腊岛北部,可以引起地震的大苏门答腊断层被分为两个部分:亚齐和Seulimeum。减少风险的一项努力是绘制断层区域的地图,特别是在地表上没有清楚显示断层标志的区域,例如印度尼西亚的Lamtamot地区。电阻率法被广泛应用于浅层结构的研究,但该方法在大面积应用时需要更多的时间。这项研究探索了极低频(极低频电磁;VLF-EM)方法对Seulimeum段浅层断层进行了研究。在此,将VLF-EM与其他地球物理方法(如电阻率法和磁法)进行了比较。为了综合结果,在地球物理研究中进行了覆盖断层露头和沟槽部位的地貌观测,以验证模型的有效性。利用数据处理,在二维剖面中显示了类似的VLF-EM和电阻率数据模式。断层结构可以在距离剖面测量值20-24 m的地方被绘制出来,这可以通过低频电磁法与导电带相关的低电流密度和电阻率的低电阻异常来证明。也可以通过磁场强度来确定断层,在距离VLF-EM和电阻率相同的距离(20-25 m)处,磁场强度显著增加。地貌观测显示出与Seulimeum段方向相同的断裂带、断裂带、断裂带等断层活动露头,而在物探测量区周围,碎块向西北方向延伸约20 m。结果表明,VLF-EM方法与其他物探和地貌观测相结合,可以作为断层成像技术,显示沿剖面20-32 m的Seulimeum断层的浅层结构。
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来源期刊
Bulletin of the Geological Society of Malaysia
Bulletin of the Geological Society of Malaysia Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
1.60
自引率
0.00%
发文量
15
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