THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA

The potential seismic hazard in the Sumatra Fault Zone (SFZ) has been highlighted as a consequence after a sequence of megathrust earthquakes in the subduction zone (2004 ????????9.2 Sumatra-Andaman, 2005 ????????8.6 Nias-Simeulue, and 2007 ????????8.4 Bengkulu). Even on the 2017 Indonesia earthq...

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Main Author: Surya Putra, Ade
Format: Dissertations
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/77506
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:77506
spelling id-itb.:775062023-09-07T14:48:55ZTHE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA Surya Putra, Ade Indonesia Dissertations Sumatran Fault Zone (SFZ), seismicity, magnitude moment, b-value, earthquake source zones INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/77506 The potential seismic hazard in the Sumatra Fault Zone (SFZ) has been highlighted as a consequence after a sequence of megathrust earthquakes in the subduction zone (2004 ????????9.2 Sumatra-Andaman, 2005 ????????8.6 Nias-Simeulue, and 2007 ????????8.4 Bengkulu). Even on the 2017 Indonesia earthquake hazard map, there are increasement report in risk hazards locally near active crustal faults, including faults with multi-segments such as SFZ. SFZ segments have been proposed through various observations such as with geological structural discontinuities, using fractal analysis as well and through seismicity using seismicity clustering. In this study we added analysis of earthquake sources by grouping each spatial change of b-values along the estimated SFZ with maximum likelihood analysis to represent the characterization of seismicity in each group. We mapped the spatial analysis of b-values using a catalogue of 681 shallow earthquakes with moment magnitudes (????????) between ????????3.0 and ????????5.6 with standard faults (????(????????)) ±0.21, estimated by applying spectral analysis methods. We get the average b-value along the SFZ quite low at 0.9 with a mean error (????????? ) of ±0.031. The lowest b-value (b = 0.74) observed in northern Sumatra (S1) and the highest b-value (b = 1.39) were in central Sumatra (S5). We analyze the pattern of changes in b-values spatially towards seismicity distribution. Based on the change in b-value, we obtain an SFZ divided into 15 earthquake source zones illustrates a pattern of seismogenic cluster and heterogeneity of the b-values. These results add to the explanation of potential seismic hazards along the SFZ segment. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description The potential seismic hazard in the Sumatra Fault Zone (SFZ) has been highlighted as a consequence after a sequence of megathrust earthquakes in the subduction zone (2004 ????????9.2 Sumatra-Andaman, 2005 ????????8.6 Nias-Simeulue, and 2007 ????????8.4 Bengkulu). Even on the 2017 Indonesia earthquake hazard map, there are increasement report in risk hazards locally near active crustal faults, including faults with multi-segments such as SFZ. SFZ segments have been proposed through various observations such as with geological structural discontinuities, using fractal analysis as well and through seismicity using seismicity clustering. In this study we added analysis of earthquake sources by grouping each spatial change of b-values along the estimated SFZ with maximum likelihood analysis to represent the characterization of seismicity in each group. We mapped the spatial analysis of b-values using a catalogue of 681 shallow earthquakes with moment magnitudes (????????) between ????????3.0 and ????????5.6 with standard faults (????(????????)) ±0.21, estimated by applying spectral analysis methods. We get the average b-value along the SFZ quite low at 0.9 with a mean error (????????? ) of ±0.031. The lowest b-value (b = 0.74) observed in northern Sumatra (S1) and the highest b-value (b = 1.39) were in central Sumatra (S5). We analyze the pattern of changes in b-values spatially towards seismicity distribution. Based on the change in b-value, we obtain an SFZ divided into 15 earthquake source zones illustrates a pattern of seismogenic cluster and heterogeneity of the b-values. These results add to the explanation of potential seismic hazards along the SFZ segment.
format Dissertations
author Surya Putra, Ade
spellingShingle Surya Putra, Ade
THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
author_facet Surya Putra, Ade
author_sort Surya Putra, Ade
title THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
title_short THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
title_full THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
title_fullStr THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
title_full_unstemmed THE CHARACTERISTICS OF EARTHQUAKE SOURCE ZONES AND DISTRIBUTION OF B VALUES ALONG THE SUMATRAN FAULT, INDONESIA
title_sort characteristics of earthquake source zones and distribution of b values along the sumatran fault, indonesia
url https://digilib.itb.ac.id/gdl/view/77506
_version_ 1822008293686509568