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Identification Lithology of Geothermal Potential Areas Using the Electrical Resistivity Tomography (ERT) Method
JURNAL GEOCELEBES · Vol. 8 No. 2 (2024) · hlm. 123–131
ISSN 2579-5546, 2579-5821
Terbit 2024-10-01
Penerbit Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Bahasa en
Abstrak
The rock lithology of the potential hydrothermal area has been studied using Electrical Resistivity Tomography (ERT) in Pungguk Pedaro Village, Bingin Kuning District, Lebong Regency. Field data acquisition uses a stretch length of 480 meter with the MAE X612-EM Geoelectric tool that forms a straight line. ERT method, using Res2dinvx64 software. The study aims to determine the subsurface conditions of the potential hydrothermal area and the characteristics of the rocks that make up the hydrothermal area. The results of this study can be concluded that Pungguk Pedaro Village is dominated by clay, sandstone, sandy gravel, andesite, basalt, and granite rocks. In this study, measurements were taken with six lines to see variations in resistivity values as a reference for identifying potential geothermal lithologies. There is 1 line that cuts to five lines to validate the resistivity value of each line. Line 1 has no potential for hydrothermal distribution because there has been a mixture of hydrothermal water with mountain water, so this line will only provide groundwater.
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University of Bengkulu Meteorological, Climatological, And Geophysical Agency Universitas Syiah Kuala
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Sumber metadata: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/geocelebes/oai, pertama di-harvest 3 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc)
<oai_dc:dc xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
<dc:title xml:lang="en">Identification Lithology of Geothermal Potential Areas Using the Electrical Resistivity Tomography (ERT) Method</dc:title>
<dc:creator xml:lang="en">Raihana, Hana</dc:creator>
<dc:creator xml:lang="en">Suhendra, Suhendra</dc:creator>
<dc:creator xml:lang="en">Nazli, Khairun</dc:creator>
<dc:creator xml:lang="en">Halauddin, Halauddin</dc:creator>
<dc:creator xml:lang="en">Refrizon, Refrizon</dc:creator>
<dc:subject xml:lang="en">ERT</dc:subject>
<dc:subject xml:lang="en">Hydrothermal</dc:subject>
<dc:subject xml:lang="en">Lebong Regency</dc:subject>
<dc:subject xml:lang="en">Lithology</dc:subject>
<dc:subject xml:lang="en">Wenner</dc:subject>
<dc:description xml:lang="en">The rock lithology of the potential hydrothermal area has been studied using Electrical Resistivity Tomography (ERT) in Pungguk Pedaro Village, Bingin Kuning District, Lebong Regency. Field data acquisition uses a stretch length of 480 meter with the MAE X612-EM Geoelectric tool that forms a straight line. ERT method, using Res2dinvx64 software. The study aims to determine the subsurface conditions of the potential hydrothermal area and the characteristics of the rocks that make up the hydrothermal area. The results of this study can be concluded that Pungguk Pedaro Village is dominated by clay, sandstone, sandy gravel, andesite, basalt, and granite rocks. In this study, measurements were taken with six lines to see variations in resistivity values as a reference for identifying potential geothermal lithologies. There is 1 line that cuts to five lines to validate the resistivity value of each line. Line 1 has no potential for hydrothermal distribution because there has been a mixture of hydrothermal water with mountain water, so this line will only provide groundwater.</dc:description>
<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
<dc:date>2024-10-01</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
<dc:format>application/pdf</dc:format>
<dc:identifier>https://journal.unhas.ac.id/index.php/geocelebes/article/view/25377</dc:identifier>
<dc:identifier>10.20956/geocelebes.v8i2.25377</dc:identifier>
<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 8 No. 2: October 2024; 123–131</dc:source>
<dc:source>2579-5546</dc:source>
<dc:source>2579-5821</dc:source>
<dc:language>en</dc:language>
<dc:relation>https://journal.unhas.ac.id/index.php/geocelebes/article/view/25377/12101</dc:relation>
<dc:rights xml:lang="en">Copyright (c) 2024 JURNAL GEOCELEBES</dc:rights>
<dc:rights xml:lang="en">https://creativecommons.org/licenses/by-nc-sa/4.0</dc:rights>
</oai_dc:dc>
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APA 7
Raihana, H., Suhendra, S., Nazli, K., Halauddin, H., & Refrizon, R. (2024). Identification Lithology of Geothermal Potential Areas Using the Electrical Resistivity Tomography (ERT) Method. JURNAL GEOCELEBES, 8(2), 123–131. https://doi.org/10.20956/geocelebes.v8i2.25377
Salin
IEEE
H. Raihana, S. Suhendra, K. Nazli, H. Halauddin, and R. Refrizon, “Identification Lithology of Geothermal Potential Areas Using the Electrical Resistivity Tomography (ERT) Method,” JURNAL GEOCELEBES, vol. 8, no. 2, pp. 123–131, 2024, doi: 10.20956/geocelebes.v8i2.25377.
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