Rita Ummi Sahida Tanjung, Dwi Pujiastuti, Ardian Putra
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引用次数: 0
摘要
本研究旨在识别磁场异常分布,以确定Sampuraga温泉周围地区的地下结构。磁场数据是用磁力计在一个面积为1400米× 1100米、有154个点的区域内测量的。测量数据为总磁场,通过日变化和IGRF校正得到磁场异常值。磁场异常值范围为353.1 nT ~ 762.2 nT。利用Oasis Montaj软件对磁场异常数据进行了极点化、向上延拓、二维建模等处理。二维模拟结果显示,研究区土壤分为三层。上部(第一和第二层)被解释为盖层。这一层由砂岩和粘土的沉积岩类型和花岗岩形式的火成岩组成,深度可达1700米。下部(第三层)被解释为储层。该层由变质沉积岩、粘土蚀变岩、安山岩熔岩、英安岩熔岩组成,深度可达地表2030 m。该模型的结果还将断裂带解释为流出带,从而在地表上形成表现。这三个地热系统的组成表明桑普拉加地区具有进一步开发和勘探的潜力。
Interpretasi Struktur Bawah Permukaan Menggunakan Data Anomali Medan Magnet Daerah Manifestasi Panas Bumi Sampuraga Kabupaten Mandailing Natal
This research was conducted to identify the distribution of magnetic field anomalies to determine the subsurface structure of the area around Sampuraga hot springs. Magnetic field data was measured using a magnetometer in an area with dimensions of 1400 m x 1100 m with 154 points. The measurement data is a total magnetic field, and to obtain magnetic field anomaly values, corrections are made for diurnal variation and IGRF correction. Magnetic field anomaly values range from 353,1 nT to 7622,0 nT. Magnetic field anomaly data were processed using the Oasis Montaj software by reducing to the poles, upward continuation, and 2D modeling. The 2D modeling results show three layers of soil in the study area. The upper part (first and second layers) is interpreted as a caprock. This layer consists of sedimentary rock types of sandstone and clay and igneous rock in the form of granite at a depth of up to 1700 m. The lower part (third layer) is interpreted as a reservoir. This layer consists of metasedimentary volcanic rock, clay alteration, andesitic lava, and dacitic lava with a depth of up to 2030 m from the ground surface. The results of this model also interpret the fault zone as an outflow zone so that it forms manifestations on the surface. These three geothermal system components show that the Sampuraga area can be further developed and explored .