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Application of Time Domain Electromagnetic Method to Study Lembang Fault, West Java

机译:时域电磁法在研究lembang断层,西爪哇省的应用

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Lembang Fault is an active fault structure lied beneath a populous area of West Java. It is located at about 9 km from the city centre of Bandung. We have conducted an electromagnetic survey in the area suggested as the zone of Lembang Fault, the Karyawangi Village, West Bandung. Time domain electromagnetic (TDEM) measurements were carried out using two profiles, with a total number of 34 soundings. The TDEM data gives detail information of the shallow conductivity structure down to a depth of 100 m. The 1-D models consist of three layers in the research area. The first layer at the depth between 0 to 3 meters is dominated by low resistivity (< 10 Ωm), which indicates the topsoil, and the second layer, considered to be tuff, which lies in the depth of 3 to 35 meters and is represented by high resistivity (> 100 Ωm). The third layer with a resistivity of 10 - 100 Ωm corresponds to sandstone. The model indicates a local fault structure in the study area.
机译:Lembang Fault是一个积极的故障结构,撒谎在西爪哇省的一个人口稠密地区。距离万隆市中心约9公里。我们在该地区进行了电磁调查,建议作为Lembang Fault,Karyawangi Village,West Bandung。使用两个型材进行时域电磁(TDEM)测量,总数为34个探测。 TDEM数据将浅电导率结构的详细信息提供到100米的深度。 1-D模型包括研究区域的三层。在0到3米之间的深度处的第一层由低电阻率(<10Ωm)主导,该电阻率(<10Ωm)表示表明,第二层被认为是凝灰岩的凝固,其位于3至35米的深度并表示通过高电阻率(>100Ωm)。电阻率为10-100Ωm的第三层对应于砂岩。该模型表示研究区域中的本地故障结构。

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