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Lembang Fault Plane Identification using Electrical Resistivity Method for Disaster Mitigation

机译:利用电阻率法灾害减缓方法的lembang断层识别

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Lembang Fault is an active fault lies from West to East located 10 kilometers in north of Bandung. It is a normal fault that its foot wall raises 40-450 meters above the ground. Its location that is not so far from Bandung, which is densely populated and frequently visited by tourists, makes Lembang Fault a threat if it becomes suddenly active. Its movement can cause earthquakes that can result in fatalities. Therefore, act of mitigation is necessary, such as educating people about Lembang Fault and its potential to cause disaster. The objective of this study is to find Lembang Fault plane below the surface with geo electrical mapping method and vertical electrical sounding method around Ciwarega and The Peak, Lembang (west side of Lembang Fault). Both of these methods are using electricity current to measure rock resistivity. Currents are injected to the ground and potential differences are measured. According to Ohm's Law, resistivity can be calculated so that resistivity distribution can be obtained. In this study, high resistivity contrast is obtained; it is about 1400-5000 Ohm.m. This resistivity contrast can be caused by lateral lithology difference resulted by fault existence. This proves that there is actually a fault in Lembang that potentially cause disasters like earthquakes.
机译:Lembang Fault是一个活跃的故障,位于万隆北部10公里的西部。它是脚壁在地面上方40-450米的正常断层。它的位置距离Bandung不远,这些位置被游客群体群体群体,使Lembang Fault成为威胁突然活跃。它的运动会导致可能导致死亡的地震。因此,需要缓解行为,例如教育人们关于lembang的错误及其造成灾难的可能性。本研究的目的是在Ciwarega和CiaWarega和峰值,lembang(Lembang Fault的西侧)周围找到lembang断层平面和垂直电气探测方法。这两种方法都使用电流来测量岩石电阻率。将电流注入地面,测量潜在的差异。根据欧姆的定律,可以计算电阻率,以便可以获得电阻率分布。在这项研究中,获得了高电阻率对比;它约为1400-5000欧姆。这种电阻率对比可以由断层存在导致的横向岩性差异引起。这证明了lembang实际上存在一个错误,可能导致地震等灾害。

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