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

JOURNAL ONLINE OF PHYSICS · Vol. 8 No. 2 (2023) · hlm. 12–22

DOI
10.22437/jop.v8i2.22184
ISSN
2502-2016
Terbit
2023-04-01
Penerbit
Prodi Fisika FST UNJA
Bahasa
en

Abstrak

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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Yosa MegasukmaAfiliasi tidak diketahui4
Jarot WiratamaAfiliasi tidak diketahui3
Aditya Denny PrabawaAfiliasi tidak diketahui2
Yudi Arista YulandaAfiliasi tidak diketahui2
Afifa Aprilia TanjungUniversitas Jambi1
Wiskandar WiskandarUniversitas Jambi1
Muhammad IkrarAfiliasi tidak diketahui1
Dimas Agung PermadiAfiliasi tidak diketahui1
Affif Farras ChanAfiliasi tidak diketahui1
Siti SadariahAfiliasi tidak diketahui1
Yudhi AchnophaUniversitas Jambi1
Nurul Izzah Asral AsralUniversitas Jambi1
Michael M.PandiaAfiliasi tidak diketahui1
Engla KardetaAfiliasi tidak diketahui1
Lenny MarlindaAfiliasi tidak diketahui1
M AL KahfiAfiliasi tidak diketahui1
Anggi Deliana SiregarAfiliasi tidak diketahui1
Wahyudi ZaharAfiliasi tidak diketahui1
Sarwo Sucitra AminAfiliasi tidak diketahui1
EricsonAfiliasi tidak diketahui1
Alkhodri RahmatullahAfiliasi tidak diketahui1
Fitri KhairunnisaAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://online-journal.unja.ac.id/index.php/jop/oai, pertama di-harvest 6 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en">MANIFESTASI PANAS BUMI SERTA REKOMENDASI PEMANFAATANNYA DI DESA KOTO SANI DAN SEKITARNYA, KECAMATAN X KOTO SINGKARAK, KABUPATEN SOLOK, PROVINSI SUMATRA BARAT </dc:title>
	<dc:creator xml:lang="en">Adhitya, Bagus</dc:creator>
	<dc:creator xml:lang="en">Ryandri Putra, Yunior</dc:creator>
	<dc:creator xml:lang="en">Ar, Arsyad</dc:creator>
	<dc:subject xml:lang="en">Geothermal Manifestations, Fluid Geochemistry, Direct Use and Indirect Use</dc:subject>
	<dc:description xml:lang="en">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.</dc:description>
	<dc:publisher xml:lang="en">Prodi Fisika FST UNJA</dc:publisher>
	<dc:date>2023-04-01</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://online-journal.unja.ac.id/jop/article/view/22184</dc:identifier>
	<dc:identifier>10.22437/jop.v8i2.22184</dc:identifier>
	<dc:source xml:lang="en">JOURNAL ONLINE OF PHYSICS; Vol. 8 No. 2 (2023): JOP (Journal Online of Physics) Vol 8 No 2; 12-22</dc:source>
	<dc:source>2502-2016</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://online-journal.unja.ac.id/jop/article/view/22184/15323</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2023 JOURNAL ONLINE OF PHYSICS</dc:rights>
</oai_dc:dc>