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Relocation of the Hypocenter of an Earthquake with the Double Difference Method in the Regional Study Area of Yogyakarta: Relokasi Hiposenter Gempabumi menggunakan Metode Double Difference Wilayah Kajian Daerah Istimewa Yogyakarta

JURNAL GEOCELEBES · Vol. 7 No. 2 (2023) · hlm. 176–185

DOI
10.20956/geocelebes.v7i2.22223
ISSN
2579-5546, 2579-5821
Terbit
2023-10-10
Penerbit
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Bahasa
en

Abstrak

The relocation of the earthquake hypocentre is necessary in order to determine the position of the earthquake centre with higher accuracy. An accurate hypocentre position is important for earthquake-prone areas mapping, seismicity analysis, and fault zone identification. The double difference algorithm technique using the hypoDD program can be used for hypocentre relocation. This article reports the earthquake relocation of 23 earthquakes in the Yogyakarta region recorded at four observation stations. The result shows that the hypocentre shift spreads randomly with a shift distance of less than 20 km, with the most shifting direction of the epicentre to the northeast. The Earthquake’s hypocentre after relocation in the land area is estimated to be triggered by a fault under the Gamping Wungkal Formation, while the earthquake around Mount Merapi is estimated to be triggered by volcanic activity. The Relocation result in the sea area show that the hypocentre leads to the subduction line.

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  • Institut Agama Islam Negeri Kendari
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Rekan penulisOrganisasiArtikel bersama
Adam ArdiansyahInstitut Agama Islam Negeri Kendari1
SarwiAfiliasi tidak diketahui1
Budi AstutiAfiliasi tidak diketahui1
Aryono AdhiAfiliasi tidak diketahui1
CindiwatiAfiliasi tidak diketahui1
Desi Mustami Limayukha Desi Mustami LimayukhaAfiliasi tidak diketahui1
Mochamad Aryono Adhi AdhiAfiliasi tidak diketahui1
Billqis El Farsiyyi Bilqis El FarsiyyiAfiliasi tidak diketahui1
Elsa Fadlika Widyantari Elsa Fadlika WidyantariAfiliasi tidak diketahui1
Ilqia Rahma Ilqia RahmaAfiliasi tidak diketahui1
Rahmania Sofyana Ulya Rahmania Sofyana UlyaAfiliasi tidak diketahui1
Adi KurniaAfiliasi tidak diketahui1

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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 3 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en">Relocation of the Hypocenter of an Earthquake with the Double Difference Method in the Regional Study Area of Yogyakarta: Relokasi Hiposenter Gempabumi menggunakan Metode Double Difference Wilayah Kajian Daerah Istimewa Yogyakarta</dc:title>
	<dc:creator xml:lang="en">Rohmiasih, Fani</dc:creator>
	<dc:creator xml:lang="en">Andi, Andi</dc:creator>
	<dc:creator xml:lang="en">Wibowo, Nugroho Budi</dc:creator>
	<dc:subject xml:lang="en">double difference</dc:subject>
	<dc:subject xml:lang="en">fault</dc:subject>
	<dc:subject xml:lang="en">hypoDD</dc:subject>
	<dc:subject xml:lang="en">residual histogram</dc:subject>
	<dc:subject xml:lang="en">subduction</dc:subject>
	<dc:description xml:lang="en">The relocation of the earthquake hypocentre is necessary in order to determine the position of the earthquake centre with higher accuracy. An accurate hypocentre position is important for earthquake-prone areas mapping, seismicity analysis, and fault zone identification. The double difference algorithm technique using the hypoDD program can be used for hypocentre relocation. This article reports the earthquake relocation of 23 earthquakes in the Yogyakarta region recorded at four observation stations. The result shows that the hypocentre shift spreads randomly with a shift distance of less than 20 km, with the most shifting direction of the epicentre to the northeast. The Earthquake’s hypocentre after relocation in the land area is estimated to be triggered by a fault under the Gamping Wungkal Formation, while the earthquake around Mount Merapi is estimated to be triggered by volcanic activity. The Relocation result in the sea area show that the hypocentre leads to the subduction line.</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2023-10-10</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/22223</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v7i2.22223</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 7 No. 2: October 2023; 176–185</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/22223/10576</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2023 JURNAL GEOCELEBES</dc:rights>
</oai_dc:dc>