Identification of Alteration Zones Based on Resistivity and Induced Polarization Geoelectric Survey

Hana Raihana, Jesika Erni Elfrita Sinaga, Adinda Gusti Cahyani, Halauddin Halauddin, Suhendra Suhendra, Anggiat Hutauruk, N. Sugianto
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Abstract

Air Putih, Lebong Regency's geothermal field, is near gold mining. The relationship between the two can be illustrated in the type of rock alteration. The study aims to identify the rock alteration zone caused by the Air Putih, Lebong Regency geothermal system. It was described by the correlation of rocks' resistivity and chargebility values based on geoelectric measurement. Two tracks spread along the Air Putih tour, with a track length of 240 meters, were used to see variations in resistivity and chargeability values and the depth of geothermal potential due to deeper current penetration to determine the alteration zone in the study area. The results of field measurements are in the form of 2D models processed with Res2DinvX64 software. According to analysis, the subsurface rock lithology in the research area is relatively the same because the location of the two measurement lines is still close together; namely, there are wet valley rocks and alterated rock layers. Pores cause rock layers found in conductive areas in the rock filled with fluid or water at high temperatures. It is evidenced by the detection of manifestations on the surface in the form of warm soil, warm rocks, steamy soil, and small holes containing water grains. The higher the temperature and pressure, the lower the value of rock-specific resistance. At the Air Putih tourist area of Lebong Regency, it is found that it is a zone of prophylitic alteration containing several minerals of andesite lava, breccia, tuff, and soil.
基于电阻率和感应极化地电测量的蚀变带识别
乐邦县的地热田Air Putih就在金矿附近。两者之间的关系可以从岩石蚀变的类型中说明。本研究旨在确定乐邦县普提空气地热系统引起的岩石蚀变带。它是通过基于地电测量的岩石电阻率和电荷率值的相关性来描述的。使用沿Air Putih之旅分布的两条轨道,轨道长度为240米,以查看电阻率和充电能力值的变化以及由于更深的电流穿透而引起的地热潜力深度,从而确定研究区域的蚀变带。现场测量的结果是用Res2DinvX64软件处理的2D模型的形式。据分析,由于两条测量线的位置仍然很近,研究区的地下岩石岩性相对相同;即有潮湿的山谷岩石和交替的岩层。孔隙导致在高温下充满流体或水的岩石中的导电区域中发现岩层。它可以通过检测到温暖的土壤、温暖的岩石、潮湿的土壤和含有水颗粒的小孔的表面表现来证明。温度和压力越高,岩石比电阻值越低。在乐邦县的Air Putih旅游区,发现了一个由安山岩熔岩、角砾岩、凝灰岩和土壤等多种矿物组成的变质带。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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