MANIFESTASI PANAS BUMI SERTA REKOMENDASI PEMANFAATANNYA DI DESA KOTO SANI DAN SEKITARNYA, KECAMATAN X KOTO SINGKARAK, KABUPATEN SOLOK, PROVINSI SUMATRA BARAT

B. Adhitya, Yunior Ryandri Putra, Arsyad Ar
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Abstract

The volcanic arc or volcanic arc that extends along the western side of Sumatra Island. Koto Sani Village, Kec. X Koto Singkarak, Solok Regency, West Sumatra Province is one of the areas on Sumatra Island that has geothermal potential. In terms of the developing tectonic order, namely in the form of a geological structure in the form of the Sumani segment of the Sumatra Fault which moves in a strike slip to the right or dextral. This geological structure is one of the main components forming the geothermal system apart from the heat source, reservoir rock, stratigraphic characteristics and the cap layer. This study aims to determine the geological setting, any geothermal manifestations found in the study area and estimate the temperature below the surface for recommendations for its use. The research method used was the interpretation of satellite imagery on the 1:25,000 scale of the Indonesian Rupa Bumi map (RBI), surface geological mapping, measurement of the physical characteristics of geothermal fluids, geochemical analysis of geothermal fluids (anion-cation) and then plotting Giggenbach's triangle diagram (1991). and geothermal geothermal calculations, as well as analysis of 18O and 2H isotopes. The research area generally forms a landscape of elongated hills with quite steep valleys as a result of tectonic activity in the form of geological structures as migration routes of hot fluids from the reservoir to the surface. This is reinforced by the results of the interpretation of river flow patterns, namely meandering or sub-dendritic and elongated or called parallel as an indication of disturbance from faults or faults. Geothermal manifestations found are hot springs, sintered silica and hydrothermal alteration rocks. The estimated temperature below the surface is 407.64°C with a high temperature category and is recommended for direct use, such as the tourism and fisheries sector, as well as indirect use, such as geothermal energy power plants.
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沿苏门答腊岛西面延伸的火山弧或火山弧。Koto Sani村,Kec。西苏门答腊省Solok Regency的X Koto Singkarak是苏门答腊岛上具有地热潜力的地区之一。就构造发育顺序而言,即以苏门答腊断裂苏马尼段的地质构造形式向右或向右走滑运动。除热源、储层、地层特征和盖层外,该地质构造是形成地热系统的主要组成部分之一。本研究旨在确定研究区域的地质背景、任何地热表现,并估计地表以下温度,为其使用提供建议。所使用的研究方法是对印度尼西亚Rupa Bumi地图(RBI) 1:25 000比例尺的卫星图像进行判读,进行地表地质填图,测量地热流体的物理特征,对地热流体进行地球化学分析(阴离子-阳离子),然后绘制Giggenbach三角形图(1991年)。地热计算,以及18O和2H同位素的分析。由于构造活动以地质构造的形式作为热流体从储层向地表迁移的通道,研究区总体上形成了细长的丘陵和相当陡峭的山谷景观。这一点得到了对河流流动模式的解释结果的加强,即蜿蜒或亚树枝状和拉长或称为平行,作为断层或断层干扰的指示。地热表现为温泉、烧结硅石和热液蚀变岩。地表以下的估计温度为407.64°C,属于高温类别,建议直接使用,如旅游和渔业部门,以及间接使用,如地热能源发电厂。
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