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Deformation Study of Papandayan Volcano using GPS Survey Method and Its Correlation with Seismic Data Observation

Journal of Engineering and Technological Sciences · Vol. 38 No. 2 (2014) · hlm. 123–146

DOI
10.5614/itbj.eng.sci.2006.38.2.4
ISSN
2338-5502, 2337-5779
Terbit
2014-01-04
Penerbit
Directorate for Research and Community Services, Institut Teknologi Bandung
Bahasa
eng

Abstrak

Papandayan volcano located in the southern part of Garut regency, around 70 km away from Bandung city, West Java. Many methods carried out to monitoring the activities of volcano, both continuously or periodically, one of the monitoring method is periodically GPS survey. Basically those surveys are carried out to understand the pattern and velocity of displacement which occurred in the volcano body, both horizontally and vertically, and also others deformation elements such as; translation, rotation and dilatation. The Mogi modeling was also used to determine the location and volume of the pressure source which caused deformation of volcano body. By comparing seismic activity and the deformation reveal from GPS measurement, before, during and after eruption, it could be understood there is a correlation between the seismicity and its deformation. These studies is hoping that GPS measurement in Papandayan volcano could be one of supported method to determine the volcano activities, at least in Papandayan volcano.

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  • Universitas Ahmad Dahlan
  • Institut Teknologi Nasional Malang
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  • Organisasi berbeda
  • Organisasi sama
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Tampilkan sebagai tabel
Rekan penulisOrganisasiArtikel bersama
M. GamalAfiliasi tidak diketahui6
Dedi MulyadiAfiliasi tidak diketahui5
Fumiaki KimataAfiliasi tidak diketahui5
Mipi A. KusumaAfiliasi tidak diketahui5
Umar RosadiAfiliasi tidak diketahui5
Iyan MulyanaAfiliasi tidak diketahui5
Bambang H. PurwantoAfiliasi tidak diketahui5
M. HendrastoAfiliasi tidak diketahui4
H. AndreasAfiliasi tidak diketahui2
M. A. KusumaAfiliasi tidak diketahui2
Sobar SutisnaAfiliasi tidak diketahui2
Dinar MaulanaAfiliasi tidak diketahui2
Oni K. SugandaAfiliasi tidak diketahui2
Buldan MuslimAfiliasi tidak diketahui2
The Houw LiongAfiliasi tidak diketahui2
Wedyanto KuntjoroAfiliasi tidak diketahui2
Cecep SubaryaAfiliasi tidak diketahui2
Hasanuddin Zainal AbidinAfiliasi tidak diketahui1
Dina Anggreni SarsitoAfiliasi tidak diketahui1
Dhota PradiptaAfiliasi tidak diketahui1
Irwan MeilanoAfiliasi tidak diketahui1
Ony K. SugandarAfiliasi tidak diketahui1
D. DarmawanAfiliasi tidak diketahui1
M. A. PurbawinataAfiliasi tidak diketahui1
A. D. WirakusumahAfiliasi tidak diketahui1
F. KimataAfiliasi tidak diketahui1
Surono SuronoUniversitas Ahmad Dahlan1
K. J. VillanuevaAfiliasi tidak diketahui1
T. PadmasariAfiliasi tidak diketahui1
Silvester Sari SaiInstitut Teknologi Nasional Malang1
O. YolandaAfiliasi tidak diketahui1
I. MeilanoAfiliasi tidak diketahui1
D. MuhardiAfiliasi tidak diketahui1
B. SetyadiAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://journals.itb.ac.id/index.php/jets/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">Deformation Study of Papandayan Volcano using GPS Survey Method and Its Correlation with Seismic Data Observation</dc:title>
	<dc:creator>Sarsito, Dina A.</dc:creator>
	<dc:creator>Andreas, Heri</dc:creator>
	<dc:creator>Abidin, Hasanuddin Z.</dc:creator>
	<dc:creator>Gamal, Muhammad</dc:creator>
	<dc:creator>Suganda, Ony K.</dc:creator>
	<dc:creator>Hendrasto, Muhammad</dc:creator>
	<dc:description xml:lang="en-US">Papandayan volcano located in the southern part of Garut regency, around 70 km away from Bandung city, West Java. Many methods carried out to monitoring the activities of volcano, both continuously or periodically, one of the monitoring method is periodically GPS survey. Basically those surveys are carried out to understand the pattern and velocity of displacement which occurred in the volcano body, both horizontally and vertically, and also others deformation elements such as; translation, rotation and dilatation. The Mogi modeling was also used to determine the location and volume of the pressure source which caused deformation of volcano body. By comparing seismic activity and the deformation reveal from GPS measurement, before, during and after eruption, it could be understood there is a correlation between the seismicity and its deformation. These studies is hoping that GPS measurement in Papandayan volcano could be one of supported method to determine the volcano activities, at least in Papandayan volcano.</dc:description>
	<dc:publisher xml:lang="en-US">Directorate for Research and Community Services, Institut Teknologi Bandung</dc:publisher>
	<dc:date>2014-01-04</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/jets/article/view/344</dc:identifier>
	<dc:identifier>10.5614/itbj.eng.sci.2006.38.2.4</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Engineering and Technological Sciences; Vol. 38 No. 2 (2006); 123-146</dc:source>
	<dc:source>2338-5502</dc:source>
	<dc:source>2337-5779</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journals.itb.ac.id/index.php/jets/article/view/344/327</dc:relation>
</oai_dc:dc>