GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008

This geodynamic analysis was analyzed based on Harvard University CMT (centroid moment tensor) solutions and from seismogram data Z, N, and E component for Sunda Strait earthquake Augustus, 26th 2008. Focal mechanism solution can be obtained from CMT and wave polarities (P, SV, and SH) which shown a...

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Main Author: HARYMURTY (NIM: 124 04 004), PRASTOWO
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/23697
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:23697
spelling id-itb.:236972017-01-24T15:47:58ZGEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008 HARYMURTY (NIM: 124 04 004), PRASTOWO Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/23697 This geodynamic analysis was analyzed based on Harvard University CMT (centroid moment tensor) solutions and from seismogram data Z, N, and E component for Sunda Strait earthquake Augustus, 26th 2008. Focal mechanism solution can be obtained from CMT and wave polarities (P, SV, and SH) which shown an oblique normal fault pattern. Vector arrays were plotted to determine the dominant force which causing the oblique normal fault pattern. Based on vector <br /> <br /> analysis performed in this study indicated that the earthquake has North-East tendency with the horizontal force is more dominant than the vertical force. From vector analysis and the location of earthquake which take place between Sumatera Fault and Mentawai fault zone can be concluded that the earthquake has a transtensional flower structure tectonic pattern. 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 This geodynamic analysis was analyzed based on Harvard University CMT (centroid moment tensor) solutions and from seismogram data Z, N, and E component for Sunda Strait earthquake Augustus, 26th 2008. Focal mechanism solution can be obtained from CMT and wave polarities (P, SV, and SH) which shown an oblique normal fault pattern. Vector arrays were plotted to determine the dominant force which causing the oblique normal fault pattern. Based on vector <br /> <br /> analysis performed in this study indicated that the earthquake has North-East tendency with the horizontal force is more dominant than the vertical force. From vector analysis and the location of earthquake which take place between Sumatera Fault and Mentawai fault zone can be concluded that the earthquake has a transtensional flower structure tectonic pattern.
format Final Project
author HARYMURTY (NIM: 124 04 004), PRASTOWO
spellingShingle HARYMURTY (NIM: 124 04 004), PRASTOWO
GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
author_facet HARYMURTY (NIM: 124 04 004), PRASTOWO
author_sort HARYMURTY (NIM: 124 04 004), PRASTOWO
title GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
title_short GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
title_full GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
title_fullStr GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
title_full_unstemmed GEODYNAMICS ANALYSIS SUNDA STRAIT EARTHQUAKE AUGUSTUS, 26 2008
title_sort geodynamics analysis sunda strait earthquake augustus, 26 2008
url https://digilib.itb.ac.id/gdl/view/23697
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