Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography

Local seismic tomography is a well-known and commonly used method for obtaining detailed information about the internal structure of volcanoes. The eruption of Mt. Agung in 2017 was a vital opportunity scientifically because it is the first eruption that had sufficient seismic observation networks t...

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Main Authors: Ardianto Ardianto, Andri Dian Nugraha, Haunan Afif, Devy Kamil Syahbana, David P. Sahara, Zulfakriza Zulfakriza, Sri Widiyantoro, Awali Priyono, Shindy Rosalia, Asep Saepuloh, Kasbani Kasbani, Faiz Muttaqy, Puput P. Rahsetyo, Imam C. Priambodo, Martanto Martanto
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.619587/full
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author Ardianto Ardianto
Andri Dian Nugraha
Andri Dian Nugraha
Haunan Afif
Devy Kamil Syahbana
David P. Sahara
Zulfakriza Zulfakriza
Zulfakriza Zulfakriza
Sri Widiyantoro
Sri Widiyantoro
Awali Priyono
Shindy Rosalia
Asep Saepuloh
Asep Saepuloh
Kasbani Kasbani
Faiz Muttaqy
Puput P. Rahsetyo
Imam C. Priambodo
Imam C. Priambodo
Martanto Martanto
Martanto Martanto
author_facet Ardianto Ardianto
Andri Dian Nugraha
Andri Dian Nugraha
Haunan Afif
Devy Kamil Syahbana
David P. Sahara
Zulfakriza Zulfakriza
Zulfakriza Zulfakriza
Sri Widiyantoro
Sri Widiyantoro
Awali Priyono
Shindy Rosalia
Asep Saepuloh
Asep Saepuloh
Kasbani Kasbani
Faiz Muttaqy
Puput P. Rahsetyo
Imam C. Priambodo
Imam C. Priambodo
Martanto Martanto
Martanto Martanto
author_sort Ardianto Ardianto
collection DOAJ
description Local seismic tomography is a well-known and commonly used method for obtaining detailed information about the internal structure of volcanoes. The eruption of Mt. Agung in 2017 was a vital opportunity scientifically because it is the first eruption that had sufficient seismic observation networks to carry out local seismic tomography at this volcano. In this study, we investigate the subsurface structure of Mt. Agung in Bali, which is one of the highest risk volcanoes in Indonesia. We conducted travel-time tomography using P- and S-wave arrival times of volcano-tectonic (VT) events to determine the three-dimensional (3D) Vp, Vs, and Vp/Vs ratio structure beneath Mt. Agung. We used 1,926 VT events, with corresponding 9482-P and 8683-S wave arrival times recorded by eight seismic stations over an observation time spanning from October 18 to December 31, 2017. We obtain the hypocenter solution for VT events using the maximum likelihood estimation algorithm and use an optimum 1D velocity model as input for the Joint 3-D seismic tomographic inversion. Local earthquake tomography revealed five anomalous regions that are useful to describe the overall seismic activity around Mt. Agung. We interpret these anomalous regions qualitatively due to limited data resolution in this study. We have successfully localized a high Vp/Vs ratio (∼1.82), low Vs (−1.9%) and high Vp (+3.8%), within a low seismicity zone at depths between 2 and 5 km below the Mt. Agung summit, which may be related to a shallow magma reservoir. There is also an anomalous region between Mt. Agung and Batur with moderate to high Vp/Vs ratios (1.76–1.79) where most of the earthquakes recorded before the 2017 eruption originated. We interpret this anomaly to be related to the existence of sub-vertical dyke complex at depths between 8 and 14 km. The results of our study provide new insights into the subsurface structure of the magma plumbing system beneath Mt. Agung, which can be used to improve the quality of determining the location of the hypocenter and source modeling for future eruption forecasting.
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spelling doaj.art-d00c49bf4a364487a1455b0dc0f5ef232022-12-21T22:11:13ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-05-01910.3389/feart.2021.619587619587Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake TomographyArdianto Ardianto0Andri Dian Nugraha1Andri Dian Nugraha2Haunan Afif3Devy Kamil Syahbana4David P. Sahara5Zulfakriza Zulfakriza6Zulfakriza Zulfakriza7Sri Widiyantoro8Sri Widiyantoro9Awali Priyono10Shindy Rosalia11Asep Saepuloh12Asep Saepuloh13Kasbani Kasbani14Faiz Muttaqy15Puput P. Rahsetyo16Imam C. Priambodo17Imam C. Priambodo18Martanto Martanto19Martanto Martanto20Geophysical Engineering Department, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Earthquake Science and Technology, Research Center for Disaster Mitigation, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Volcanology and Geological Hazards Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Bandung, IndonesiaCenter for Volcanology and Geological Hazards Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Earthquake Science and Technology, Research Center for Disaster Mitigation, Institut Teknologi Bandung, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaFaculty of Engineering, Maranatha Christian University, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaGlobal Geophysics Research Group, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Remote Sensing, Institut Teknologi Bandung, Bandung, IndonesiaGeology Engineering Study Program, Faculty of Earth Sciences and Technology, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Volcanology and Geological Hazards Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Bandung, IndonesiaGeophysical Engineering Department, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaGeophysical Engineering Department, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaGeophysical Engineering Department, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Volcanology and Geological Hazards Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Bandung, IndonesiaGeophysical Engineering Department, Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Bandung, IndonesiaCenter for Volcanology and Geological Hazards Mitigation, Geological Agency, Ministry of Energy and Mineral Resources, Bandung, IndonesiaLocal seismic tomography is a well-known and commonly used method for obtaining detailed information about the internal structure of volcanoes. The eruption of Mt. Agung in 2017 was a vital opportunity scientifically because it is the first eruption that had sufficient seismic observation networks to carry out local seismic tomography at this volcano. In this study, we investigate the subsurface structure of Mt. Agung in Bali, which is one of the highest risk volcanoes in Indonesia. We conducted travel-time tomography using P- and S-wave arrival times of volcano-tectonic (VT) events to determine the three-dimensional (3D) Vp, Vs, and Vp/Vs ratio structure beneath Mt. Agung. We used 1,926 VT events, with corresponding 9482-P and 8683-S wave arrival times recorded by eight seismic stations over an observation time spanning from October 18 to December 31, 2017. We obtain the hypocenter solution for VT events using the maximum likelihood estimation algorithm and use an optimum 1D velocity model as input for the Joint 3-D seismic tomographic inversion. Local earthquake tomography revealed five anomalous regions that are useful to describe the overall seismic activity around Mt. Agung. We interpret these anomalous regions qualitatively due to limited data resolution in this study. We have successfully localized a high Vp/Vs ratio (∼1.82), low Vs (−1.9%) and high Vp (+3.8%), within a low seismicity zone at depths between 2 and 5 km below the Mt. Agung summit, which may be related to a shallow magma reservoir. There is also an anomalous region between Mt. Agung and Batur with moderate to high Vp/Vs ratios (1.76–1.79) where most of the earthquakes recorded before the 2017 eruption originated. We interpret this anomaly to be related to the existence of sub-vertical dyke complex at depths between 8 and 14 km. The results of our study provide new insights into the subsurface structure of the magma plumbing system beneath Mt. Agung, which can be used to improve the quality of determining the location of the hypocenter and source modeling for future eruption forecasting.https://www.frontiersin.org/articles/10.3389/feart.2021.619587/fullseismic tomographyMt. Agungmagma plumbing system3D seismic structurevolcano seismology
spellingShingle Ardianto Ardianto
Andri Dian Nugraha
Andri Dian Nugraha
Haunan Afif
Devy Kamil Syahbana
David P. Sahara
Zulfakriza Zulfakriza
Zulfakriza Zulfakriza
Sri Widiyantoro
Sri Widiyantoro
Awali Priyono
Shindy Rosalia
Asep Saepuloh
Asep Saepuloh
Kasbani Kasbani
Faiz Muttaqy
Puput P. Rahsetyo
Imam C. Priambodo
Imam C. Priambodo
Martanto Martanto
Martanto Martanto
Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
Frontiers in Earth Science
seismic tomography
Mt. Agung
magma plumbing system
3D seismic structure
volcano seismology
title Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
title_full Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
title_fullStr Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
title_full_unstemmed Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
title_short Imaging the Subsurface Structure of Mount Agung in Bali (Indonesia) Using Volcano-Tectonic (VT) Earthquake Tomography
title_sort imaging the subsurface structure of mount agung in bali indonesia using volcano tectonic vt earthquake tomography
topic seismic tomography
Mt. Agung
magma plumbing system
3D seismic structure
volcano seismology
url https://www.frontiersin.org/articles/10.3389/feart.2021.619587/full
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