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APPLICATION INTEGRATION METHODS ON LANDSAT ETM + TO DETERMINE EARTHQUAKE POTENTIALS IN PALU GRABEN

Indonesian Journal of Geography · Vol. 42 No. 1 (2010) · hlm. 91–104

DOI
10.22146/ijg.1579
ISSN
2354-9114, 0024-9521
Terbit
2010-06-01
Penerbit
Faculty of Geography, Universitas Gadjah Mada
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-nc/4.0

Abstrak

This study aims to assess the ability of the integration method at LandsatETM + imagery in recognizing object fault, main fault and secondary fault in PaluGraben. Mapping of fault and calculate earthquake potential, based of fault that isfound in Graben of Palu. The image used in this study is Landsat ETM +.Techniques used to process Landsat ETM + is a method of integration. LandsatETM+ imagery processed with ENVI software 4.4, while the mapping of faults anddetermining of length using ArcGIS 9.2.The potential of earthquakes is calculatedfrom the length of faults found in the Graben of Palu. Results obtained showed thatthe patterns of lineament as a picture of fault in the Palu Graben can be extractedfrom Landsat ETM +. Lineament of fault is seen clearly on Landsat ETM + imageprocessed with integration method and band combination, 45PC1_8. Faults arearranged in the form of map. There are 66 faults found at research sites.Magnitude earthquake 5,5 SR can be produced from the fault with a length greaterthan or equal to 9 km. If each faults contributes the same to earthquakeoccurrence, the potential incidence of earthquake with magnitude greater than orequal to 5.5 SR in the Graben of Palu is 33.8%, while the magnitude is smallerthan 5.5 SR is 66.2%. The largest magnitude that can occur in Palu Graben, 7.1SR. These results indicate that the potential earthquake destructive (≥ 5.5 SR) ofapproximately 33.8%.

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  • Padjadjaran University
  • Universitas Gadjah Mada
  • Tadulako University
  • Sumatera Institute of Technology
  • Ministry of Marine Affairs and Fisheries
  • Universitas Muhammadiyah Sumatera Utara
  • Sebelas Maret University
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Rekan penulisOrganisasiArtikel bersama
Junun SartohadiUniversitas Gadjah Mada2
Mochamad Rudyansyah IsmailPadjadjaran University2
Rizki Dimas PermanaSumatera Institute of Technology1
Syawalludin Alisyahbana HarahapPadjadjaran University1
Indah RiyantiniPadjadjaran University1
Yuwanda IlhamMinistry of Marine Affairs and Fisheries1
Puspita Indra WardhaniUniversitas Gadjah Mada1
Suwarno SuwarnoUniversitas Muhammadiyah Sumatera Utara1
Djarot SadhartoUniversitas Gadjah Mada1
Winesti TubagusPadjadjaran University1
Lintang Permata Sari YuliadiPadjadjaran University1
Syawaludin Alisyahbana HarahapPadjadjaran University1
Ibnu FaizalPadjadjaran University1
Muhammad IrhasPadjadjaran University1
Hartono HartonoSebelas Maret University1
Ardhasena SopaheluwakanMeteorological, Climatological, And Geophysical Agency1
Ida PramuwardaniUniversitas Gadjah Mada1

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Sumber metadata: OAI-PMH (metadata jurnal) http://jurnal.ugm.ac.id/ijg/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">APPLICATION INTEGRATION METHODS ON LANDSAT ETM + TO DETERMINE EARTHQUAKE POTENTIALS IN PALU GRABEN</dc:title>
	<dc:creator>H, M. Rusydi</dc:creator>
	<dc:creator>Hartono, Hartono</dc:creator>
	<dc:creator>Hadi, M. Pramono</dc:creator>
	<dc:creator>Sunarto, Sunarto</dc:creator>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:subject xml:lang="en-US">integration, Landsat ETM +, earthquake, Palu Graben</dc:subject>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:description xml:lang="en-US">This study aims to assess the ability of the integration method at LandsatETM + imagery in recognizing object fault, main fault and secondary fault in PaluGraben. Mapping of fault and calculate earthquake potential, based of fault that isfound in Graben of Palu. The image used in this study is Landsat ETM +.Techniques used to process Landsat ETM + is a method of integration. LandsatETM+ imagery processed with ENVI software 4.4, while the mapping of faults anddetermining of length using ArcGIS 9.2.The potential of earthquakes is calculatedfrom the length of faults found in the Graben of Palu. Results obtained showed thatthe patterns of lineament as a picture of fault in the Palu Graben can be extractedfrom Landsat ETM +. Lineament of fault is seen clearly on Landsat ETM + imageprocessed with integration method and band combination, 45PC1_8. Faults arearranged in the form of map. There are 66 faults found at research sites.Magnitude earthquake 5,5 SR can be produced from the fault with a length greaterthan or equal to 9 km. If each faults contributes the same to earthquakeoccurrence, the potential incidence of earthquake with magnitude greater than orequal to 5.5 SR in the Graben of Palu is 33.8%, while the magnitude is smallerthan 5.5 SR is 66.2%. The largest magnitude that can occur in Palu Graben, 7.1SR. These results indicate that the potential earthquake destructive (≥ 5.5 SR) ofapproximately 33.8%.</dc:description>
	<dc:publisher xml:lang="en-US">Faculty of Geography, Universitas Gadjah Mada</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2010-06-01</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-US">Peer-reviewed Article</dc:type>
	<dc:type xml:lang="en-US"></dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.ugm.ac.id/ijg/article/view/1579</dc:identifier>
	<dc:identifier>10.22146/ijg.1579</dc:identifier>
	<dc:source xml:lang="en-US">Indonesian Journal of Geography; Vol 42, No 1 (2010): Indonesian Journal of Geography; 91-104</dc:source>
	<dc:source>2354-9114</dc:source>
	<dc:source>0024-9521</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journal.ugm.ac.id/ijg/article/view/1579/pdf_12</dc:relation>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:rights xml:lang="en-US">Copyright (c) 2010 Indonesian Journal of Geography</dc:rights>
	<dc:rights xml:lang="en-US">http://creativecommons.org/licenses/by-nc/4.0</dc:rights>
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