HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015

Gede volcano is an active volcano in West Java, Indonesia.  Research about determination the volcano-tectonic earthquake source positions has given results using volcano-tectonic earthquakes data from January until November 2015. Volcano-tectonic earthquakes contained deep (VT-A) have frequency (max...

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Main Authors: Aulia Kharisma Nugraha, Sukir Maryanto, Hetty Triastuty
Format: Article
Language:English
Published: Jurusan Fisika Fakultas Sains Dan Teknologi, Universitas Islam Negeri Maulana Malik Ibrahim Malang 2017-04-01
Series:Jurnal Neutrino: Jurnal Fisika dan Aplikasinya
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Online Access:http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/4103
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author Aulia Kharisma Nugraha
Sukir Maryanto
Hetty Triastuty
author_facet Aulia Kharisma Nugraha
Sukir Maryanto
Hetty Triastuty
author_sort Aulia Kharisma Nugraha
collection DOAJ
description Gede volcano is an active volcano in West Java, Indonesia.  Research about determination the volcano-tectonic earthquake source positions has given results using volcano-tectonic earthquakes data from January until November 2015. Volcano-tectonic earthquakes contained deep (VT-A) have frequency (maximum amplitude) range 5 – 15 Hz. Furthermore, they contain shallow earthquake, VT-B have range 3-5 Hz and LF have range 1-3 Hz. Geiger’s Adaptive Damping (GAD) methods used for determining the hypocenter of these volcano-tectonic (VT) events. Hypocenter distribution divided into 4 clusters. Cluster I located in the crater of Gede volcano dominated by VT-B earthquakes their depth range 2 km below MSL to 2 km above MSL including the VT-B swarm. The seismic sources in cluster I indicated dominant due to the volcanic fluid or gas filled in conduit pipes. Cluster II located at the west of Gede volcano caused by Gede-Pangrango fault-line dominated by VT-A earthquakes with depths range 1.5 km below MSL to 700 m above MSL. Cluster III located in the North of Gede volcano dominated by VT-A events there caused by graben fault area with those depths range 7.5 – 1.65 km below MSL. Cluster IV located in South West of Gede volcano contained VT-A earthquakes with depth range at 10 km below MSL and VT-B earthquakes this depth 2 km below MSL. Due to magma intrusion filled into fractures of the fault in the West of Gede volcano this shallow magma filling-fractures and degassing in subsurface assumed dominates the volcano-tectonic events from January to November 2015 due to faults extends from North to South occured in the West of Gede volcano.
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institution Kabale University
issn 1979-6374
2460-5999
language English
publishDate 2017-04-01
publisher Jurusan Fisika Fakultas Sains Dan Teknologi, Universitas Islam Negeri Maulana Malik Ibrahim Malang
record_format Article
series Jurnal Neutrino: Jurnal Fisika dan Aplikasinya
spelling doaj-art-e2db4e5e043f43f4ad327db33d312a122024-12-02T04:17:38ZengJurusan Fisika Fakultas Sains Dan Teknologi, Universitas Islam Negeri Maulana Malik Ibrahim MalangJurnal Neutrino: Jurnal Fisika dan Aplikasinya1979-63742460-59992017-04-0192445110.18860/neu.v9i2.41033371HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015Aulia Kharisma Nugraha0Sukir Maryanto1Hetty Triastuty2Magister of Physics Faculty of Mathematics and Natural Sciences Brawijaya UniversityPhysics Department Faculty of Mathematics and Natural Sciences Brawijaya UniversityCenter of Volcanology and Geological Hazard MitigationGede volcano is an active volcano in West Java, Indonesia.  Research about determination the volcano-tectonic earthquake source positions has given results using volcano-tectonic earthquakes data from January until November 2015. Volcano-tectonic earthquakes contained deep (VT-A) have frequency (maximum amplitude) range 5 – 15 Hz. Furthermore, they contain shallow earthquake, VT-B have range 3-5 Hz and LF have range 1-3 Hz. Geiger’s Adaptive Damping (GAD) methods used for determining the hypocenter of these volcano-tectonic (VT) events. Hypocenter distribution divided into 4 clusters. Cluster I located in the crater of Gede volcano dominated by VT-B earthquakes their depth range 2 km below MSL to 2 km above MSL including the VT-B swarm. The seismic sources in cluster I indicated dominant due to the volcanic fluid or gas filled in conduit pipes. Cluster II located at the west of Gede volcano caused by Gede-Pangrango fault-line dominated by VT-A earthquakes with depths range 1.5 km below MSL to 700 m above MSL. Cluster III located in the North of Gede volcano dominated by VT-A events there caused by graben fault area with those depths range 7.5 – 1.65 km below MSL. Cluster IV located in South West of Gede volcano contained VT-A earthquakes with depth range at 10 km below MSL and VT-B earthquakes this depth 2 km below MSL. Due to magma intrusion filled into fractures of the fault in the West of Gede volcano this shallow magma filling-fractures and degassing in subsurface assumed dominates the volcano-tectonic events from January to November 2015 due to faults extends from North to South occured in the West of Gede volcano.http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/4103Gedevolcanovolcano-tectonicearthquakehypocenter
spellingShingle Aulia Kharisma Nugraha
Sukir Maryanto
Hetty Triastuty
HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
Jurnal Neutrino: Jurnal Fisika dan Aplikasinya
Gede
volcano
volcano-tectonic
earthquake
hypocenter
title HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
title_full HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
title_fullStr HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
title_full_unstemmed HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
title_short HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015
title_sort hypocenter determination and clustering of volcano tectonic earthquakes in gede volcano 2015
topic Gede
volcano
volcano-tectonic
earthquake
hypocenter
url http://ejournal.uin-malang.ac.id/index.php/NEUTRINO/article/view/4103
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AT hettytriastuty hypocenterdeterminationandclusteringofvolcanotectonicearthquakesingedevolcano2015