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Source Processes of the March 2007 Singkarak Earthquakes Inferred from Teleseismic Data

Journal of Mathematical and Fundamental Sciences · Vol. 46 No. 2 (2014) · hlm. 159–168

DOI
10.5614/j.math.fund.sci.2014.46.2.4
ISSN
2338-5510, 2337-5760
Terbit
2014-07-01
Penerbit
Directorate for Research and Innovation (DRI) ITB
Bahasa
eng

Abstrak

The rupture processes of two sequentialearthquakes have been inverted from teleseismic data. The first event released a total seismic moment of 7.9×1018 Nm (Mw 6.5) and the slip distribution shows three asperities, 1.5 m at the shallowside, 0.7 m at the rightsouth-east deep side and 0.5 m atthe north-west deep side. The second event had one asperity with 1.7 m slip and released a seismic moment of 7.5×1018 Nm (Mw 6.5). In both cases, maximum slip occurred above the hypocenter which was responsible for the surface displacement pattern.

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  • Bandung Institute of Technology
  • Kagoshima University
  • Indonesian Institute of Sciences
  • Tokyo Institute of Technology
  • Meteorological, Climatological, And Geophysical Agency
  • Hasanuddin University
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Rekan penulisOrganisasiArtikel bersama
Hiroaki YamanakaTokyo Institute of Technology2
Masyhur IrsyamBandung Institute of Technology1
Sri WidiyantoroBandung Institute of Technology1
Mohamad RidwanBandung Institute of Technology1
Andri Dian NugrahaBandung Institute of Technology1
Ahmad SyahputraBandung Institute of Technology1
Nanang T. PuspitoBandung Institute of Technology1
Sugeng PribadiMeteorological, Climatological, And Geophysical Agency1
Gunawan IbrahimBandung Institute of Technology1
Andi Muhamad PramatadieHasanuddin University1

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Sumber metadata: OAI-PMH (metadata jurnal) https://journals.itb.ac.id/index.php/jmfs/oai, pertama di-harvest 9 Nov 2026, terakhir terlihat 9 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en-US">Source Processes of the March 2007 Singkarak Earthquakes Inferred from Teleseismic Data</dc:title>
	<dc:creator>Afnimar, A.</dc:creator>
	<dc:creator>Kobayashi, Reiji</dc:creator>
	<dc:creator>Natawidjaja, Danny Hilman</dc:creator>
	<dc:subject xml:lang="en-US">asperity</dc:subject>
	<dc:subject xml:lang="en-US">source process</dc:subject>
	<dc:subject xml:lang="en-US">shallow rupture</dc:subject>
	<dc:subject xml:lang="en-US">surface displacement</dc:subject>
	<dc:subject xml:lang="en-US">teleseismic data</dc:subject>
	<dc:description xml:lang="en-US">The rupture processes of two sequentialearthquakes have been inverted from teleseismic data. The first event released a total seismic moment of 7.9×1018 Nm (Mw 6.5) and the slip distribution shows three asperities, 1.5 m at the shallowside, 0.7 m at the rightsouth-east deep side and 0.5 m atthe north-west deep side. The second event had one asperity with 1.7 m slip and released a seismic moment of 7.5×1018 Nm (Mw 6.5). In both cases, maximum slip occurred above the hypocenter which was responsible for the surface displacement pattern.</dc:description>
	<dc:publisher xml:lang="en-US">Directorate for Research and Innovation (DRI) ITB</dc:publisher>
	<dc:date>2014-07-01</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journals.itb.ac.id/index.php/jmfs/article/view/824</dc:identifier>
	<dc:identifier>10.5614/j.math.fund.sci.2014.46.2.4</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Mathematical and Fundamental Sciences; Vol. 46 No. 2 (2014); 159-168</dc:source>
	<dc:source>2338-5510</dc:source>
	<dc:source>2337-5760</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journals.itb.ac.id/index.php/jmfs/article/view/824/502</dc:relation>
</oai_dc:dc>