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Identification of subsurface fault using schlumberger configuration geoelectricity method. Case study in Opak River Yogyakarta

INDONESIAN JOURNAL OF APPLIED PHYSICS · Vol. 5 No. 02 (2015) · hlm. 10–24

DOI
10.13057/ijap.v5i02.278
ISSN
2477-6416, 2089-0133
Terbit
2015-12-20
Penerbit
Department of Physics, Sebelas Maret University
Bahasa
eng

Abstrak

The Opak river is formed by fault. The earthquake in Yogyakarta on May 27th, 2006 had activated the Opak’s fault and caused secondary fault. The fault had made destruction of the infrastructure. This research aimed to determine the description of subsurface structure and to identify the location of the underground fault. The Schlumberger configuration of geoelectrical method was used for identifying the fault in the research area. The data collected in three lines of each which the length is 75 meters. The datas were processed by Res2dinv and Surfer 10.0. Based on the result of the process, the resistivity value are 5-1077 Ωm and the discontinue plane of the contour profile resistivity at depth function. The discontinuities of resistivity value can be interpreted the fault plane. The position of the fault in line A is 38 m, while on the line B and C, the fault locations are located at 33 m from the start point of the measurement. The faults in lines A, B, and C are straight with the strike N 113° E.

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  • State University of Semarang
  • IAIN Syekh Nurjati Cirebon
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Rekan penulisOrganisasiArtikel bersama
KhumaediState University of Semarang3
Susilo SusiloState University of Semarang2
Fianti FiantiAfiliasi tidak diketahui2
Suharto LinuwihAfiliasi tidak diketahui1
Yunita Putri SuyantoAfiliasi tidak diketahui1
Ngurah Made Darma PutraState University of Semarang1
ErnawatiAfiliasi tidak diketahui1
Ani RusilowatiState University of Semarang1
Meili SusantiAfiliasi tidak diketahui1
Achmad SopyanAfiliasi tidak diketahui1
Fitroh Imam AchmadAfiliasi tidak diketahui1
Fayeza CamaliaAfiliasi tidak diketahui1
Azhari MunifAfiliasi tidak diketahui1
Nathan HindartoState University of Semarang1
Yogi PrabowoAfiliasi tidak diketahui1
Sekar RachmawatiState University of Semarang1
Putut MarwotoState University of Semarang1
Ismira Wahyu Lestari LewaAfiliasi tidak diketahui1
Budi Naini MindyartoAfiliasi tidak diketahui1
Astri Setia NingrumAfiliasi tidak diketahui1
Sugianto SugiantoIAIN Syekh Nurjati Cirebon1
Try Lysa HandayaniAfiliasi tidak diketahui1
Elly UzaedahAfiliasi tidak diketahui1
sunyoto eko nugrohoState University of Semarang1
Riza Isnaini NingtyasAfiliasi tidak diketahui1
Retno PurwaningsihAfiliasi tidak diketahui1
Ismi LutfinurAfiliasi tidak diketahui1
Rulyaimah RulyaimahAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://jurnal.uns.ac.id/ijap/oai, pertama di-harvest 8 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en-US">Identification of subsurface fault using schlumberger configuration geoelectricity method. Case study in Opak River Yogyakarta</dc:title>
	<dc:creator>Lutfinur, Ismi</dc:creator>
	<dc:creator>K, Khumaedi</dc:creator>
	<dc:creator>Susanto, Hadi</dc:creator>
	<dc:description xml:lang="en-US">The Opak river is formed by fault. The earthquake in Yogyakarta on May 27th, 2006 had activated the Opak’s fault and caused secondary fault. The fault had made destruction of the infrastructure. This research aimed to determine the description of subsurface structure and to identify the location of the underground fault. The Schlumberger configuration of geoelectrical method was used for identifying the fault in the research area. The data collected in three lines of each which the length is 75 meters. The datas were processed by Res2dinv and Surfer 10.0. Based on the result of the process, the resistivity value are 5-1077 Ωm and the discontinue plane of the contour profile resistivity at depth function. The discontinuities of resistivity value can be interpreted the fault plane. The position of the fault in line A is 38 m, while on the line B and C, the fault locations are located at 33 m from the start point of the measurement. The faults in lines A, B, and C are straight with the strike N 113° E.</dc:description>
	<dc:publisher xml:lang="en-US">Department of Physics, Sebelas Maret University</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2015-12-20</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-US">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jurnal.uns.ac.id/ijap/article/view/278</dc:identifier>
	<dc:identifier>10.13057/ijap.v5i02.278</dc:identifier>
	<dc:source xml:lang="en-US">INDONESIAN JOURNAL OF APPLIED PHYSICS; Vol 5, No 02 (2015): October; 10-24</dc:source>
	<dc:source>2477-6416</dc:source>
	<dc:source>2089-0133</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://jurnal.uns.ac.id/ijap/article/view/278/254</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2015 INDONESIAN JOURNAL OF APPLIED PHYSICS</dc:rights>
</oai_dc:dc>