Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia

Sukir Maryanto

doi:10.1063/1.5061870

Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia

Sukir Maryanto^*

^*Corresponding author for this work

Faculty of Mathematics and Natural Sciences

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

4 Citations (Scopus)

Abstract

Microseismicity was investigated around the Cangar, Arjuno-Welirang volcano-hosted geothermal complex. The goals were to determine the distribution of the epicenter and hypocenter of a microearthquake that changed in spatio-temporal and distribution of Peak Ground Acceleration (PGA). To determine the epicenter and hypocenter, analysis of the frequency spectrum was applied to seismic signals to determine the range of dominant frequency values of the event. Then, it was filtered by the band-pass filter to get the original signal of the event. This research obtained a microseismic frequency in the range of 12-24 Hz, depth of the shallow source in the range of 4-264 meters, while the deeper sources were located at a depth of 985-2152 meters. The distribution of PGA values around the Arjuno-Welirang volcanic complex was in the range of 15.02-21.80 Gal.

Original language	English
Title of host publication	9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University
Editors	Fahrul Zaman Bin Huyop, Dian Siswanto, Retno Mastuti, Chairat Treesubsuntorn
Publisher	American Institute of Physics Inc.
ISBN (Electronic)	9780735417373
DOIs	https://doi.org/10.1063/1.5061870
Publication status	Published - 10 Oct 2018
Event	9th International Conference on Global Resource Conservation and AJI from Ritsumeikan University, ICGRC 2018 - Malang City - East Java, Indonesia Duration: 7 Mar 2018 → 8 Mar 2018

Publication series

Name	AIP Conference Proceedings
Volume	2019
ISSN (Print)	0094-243X
ISSN (Electronic)	1551-7616

Conference

Conference	9th International Conference on Global Resource Conservation and AJI from Ritsumeikan University, ICGRC 2018
Country/Territory	Indonesia
City	Malang City - East Java
Period	7/03/18 → 8/03/18

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 11 Sustainable Cities and Communities

Keywords

epicenter
hypocenter
microseismicity

Access to Document

10.1063/1.5061870

Cite this

Maryanto, S. (2018). Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia. In F. Z. B. Huyop, D. Siswanto, R. Mastuti, & C. Treesubsuntorn (Eds.), 9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University Article 030017 (AIP Conference Proceedings; Vol. 2019). American Institute of Physics Inc.. https://doi.org/10.1063/1.5061870

Maryanto, Sukir. / Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia. 9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University. editor / Fahrul Zaman Bin Huyop ; Dian Siswanto ; Retno Mastuti ; Chairat Treesubsuntorn. American Institute of Physics Inc., 2018. (AIP Conference Proceedings).

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title = "Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia",

abstract = "Microseismicity was investigated around the Cangar, Arjuno-Welirang volcano-hosted geothermal complex. The goals were to determine the distribution of the epicenter and hypocenter of a microearthquake that changed in spatio-temporal and distribution of Peak Ground Acceleration (PGA). To determine the epicenter and hypocenter, analysis of the frequency spectrum was applied to seismic signals to determine the range of dominant frequency values of the event. Then, it was filtered by the band-pass filter to get the original signal of the event. This research obtained a microseismic frequency in the range of 12-24 Hz, depth of the shallow source in the range of 4-264 meters, while the deeper sources were located at a depth of 985-2152 meters. The distribution of PGA values around the Arjuno-Welirang volcanic complex was in the range of 15.02-21.80 Gal.",

keywords = "epicenter, hypocenter, microseismicity",

author = "Sukir Maryanto",

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Maryanto, S 2018, Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia. in FZB Huyop, D Siswanto, R Mastuti & C Treesubsuntorn (eds), 9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University., 030017, AIP Conference Proceedings, vol. 2019, American Institute of Physics Inc., 9th International Conference on Global Resource Conservation and AJI from Ritsumeikan University, ICGRC 2018, Malang City - East Java, Indonesia, 7/03/18. https://doi.org/10.1063/1.5061870

Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia. / Maryanto, Sukir.
9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University. ed. / Fahrul Zaman Bin Huyop; Dian Siswanto; Retno Mastuti; Chairat Treesubsuntorn. American Institute of Physics Inc., 2018. 030017 (AIP Conference Proceedings; Vol. 2019).

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

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AU - Maryanto, Sukir

PY - 2018/10/10

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N2 - Microseismicity was investigated around the Cangar, Arjuno-Welirang volcano-hosted geothermal complex. The goals were to determine the distribution of the epicenter and hypocenter of a microearthquake that changed in spatio-temporal and distribution of Peak Ground Acceleration (PGA). To determine the epicenter and hypocenter, analysis of the frequency spectrum was applied to seismic signals to determine the range of dominant frequency values of the event. Then, it was filtered by the band-pass filter to get the original signal of the event. This research obtained a microseismic frequency in the range of 12-24 Hz, depth of the shallow source in the range of 4-264 meters, while the deeper sources were located at a depth of 985-2152 meters. The distribution of PGA values around the Arjuno-Welirang volcanic complex was in the range of 15.02-21.80 Gal.

AB - Microseismicity was investigated around the Cangar, Arjuno-Welirang volcano-hosted geothermal complex. The goals were to determine the distribution of the epicenter and hypocenter of a microearthquake that changed in spatio-temporal and distribution of Peak Ground Acceleration (PGA). To determine the epicenter and hypocenter, analysis of the frequency spectrum was applied to seismic signals to determine the range of dominant frequency values of the event. Then, it was filtered by the band-pass filter to get the original signal of the event. This research obtained a microseismic frequency in the range of 12-24 Hz, depth of the shallow source in the range of 4-264 meters, while the deeper sources were located at a depth of 985-2152 meters. The distribution of PGA values around the Arjuno-Welirang volcanic complex was in the range of 15.02-21.80 Gal.

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KW - hypocenter

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Y2 - 7 March 2018 through 8 March 2018

ER -

Maryanto S. Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia. In Huyop FZB, Siswanto D, Mastuti R, Treesubsuntorn C, editors, 9th International Conference on Global Resource Conservation, ICGRC and AJI from Ritsumeikan University. American Institute of Physics Inc. 2018. 030017. (AIP Conference Proceedings). doi: 10.1063/1.5061870

Microseismicity recorded at Cangar, Arjuno-Welirang volcano-hosted geothermal complex, Batu City, East Java, Indonesia

Abstract

Publication series

Conference

UN SDGs

Keywords

Access to Document

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