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turnitin Identifikasi Batuan Andesit Menggunakan Metode Geolistrik 2D di Daerah Pengaron, Kalimantan Selatan

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dc.contributor.author Simamora, Selvy Tiurma
dc.contributor.author Wahyono, Sri Cahyo
dc.contributor.author Siregar, Simon Sadok
dc.date.accessioned 2022-04-26T03:39:37Z
dc.date.available 2022-04-26T03:39:37Z
dc.date.issued 2020-10-01
dc.identifier.issn 2302-8491
dc.identifier.issn 2686-2433
dc.identifier.uri https://repo-dosen.ulm.ac.id//handle/123456789/23980
dc.description.abstract Research has been carried out to identify andesite rock layers using 2D geoelectrical method with Schlumberger configuration in the Pengaron area, South Kalimantan. Measurements were made for five tracks with a length of each track being 270 m. The purpose of this research is to model the cross section of 2D resistivity values, determine the type of lithology, depth and thickness of andesite rocks in the study area. Based on the results of data processing, three layers of rock types were obtained. The first layer is the top soil layer with a resistivity value of 39–116 Ωm, the second layer is clay with a resistivity value of 143–298 Ωm and the third layer is andesite rock with a resistivity value of 320–1,000 Ωm. The 2D interpretation results show that andesite rocks have a resistivity value of 382–1,000 Ωm at a depth of 10-77 m and a thickness of 10–55 m. en_US
dc.language.iso en en_US
dc.publisher 'Jurusan Fisika, FMIPA Universitas Andalas en_US
dc.subject andesite rock geoelectrical method Schlumberger configuration Pengaron area en_US
dc.title turnitin Identifikasi Batuan Andesit Menggunakan Metode Geolistrik 2D di Daerah Pengaron, Kalimantan Selatan en_US
dc.type Article en_US


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