COSEISMIC ANALISYS 2007 SIANOK EARTHQUAKE BASE ON GPS OBSERVATION FROM 1993-2007
Sumatra island is a part of Eurasian plate that has convergence interraction with <br /> <br /> <br /> <br /> Indo-Australian plate. Oblique subduction between those plates forming a <br /> <br /> <br /> <br /> subduction zone in the western pa...
Saved in:
Main Author: | |
---|---|
Format: | Theses |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/22713 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Sumatra island is a part of Eurasian plate that has convergence interraction with <br />
<br />
<br />
<br />
Indo-Australian plate. Oblique subduction between those plates forming a <br />
<br />
<br />
<br />
subduction zone in the western part of the Sumatran island and fault segments <br />
<br />
<br />
<br />
onshore Sumatra island. Those subduction zones and fault segments often cause <br />
<br />
<br />
<br />
earthquakes in the region. <br />
<br />
<br />
<br />
Since the introduction of the Indonesia Geospatial Reference System 2013 <br />
<br />
<br />
<br />
(IGRS2013) as a geodetic datum for mapping activity in Indonesia, the change of <br />
<br />
<br />
<br />
reference frame position as a function of time due to the dynamics of the earth needs <br />
<br />
<br />
<br />
to be taken into account. The occurrence of two consecutive earthquakes on March <br />
<br />
<br />
<br />
6, 2007 in the Lake Singkarak, West Sumatra (Sianok Earthquake), lead a coseismic <br />
<br />
<br />
<br />
deformation that affect the IGRS2013. In this study, an analysis performed to <br />
<br />
<br />
<br />
determine the most appropriate co-seismic deformation model of the Sianok <br />
<br />
<br />
<br />
earthquake and the extent of its impact on IGRS2013. <br />
<br />
<br />
<br />
Based on the analysis of validation residual value at 11 GPS stations, can be <br />
<br />
<br />
<br />
concluded that the most appropriate co-seismic deformation model of the Sianok <br />
<br />
<br />
<br />
earthquake is the model developed using earthquake parameter data derived from <br />
<br />
<br />
<br />
Global CMT with residual misfit 47.5 mm. The magnitude of the coseismic <br />
<br />
<br />
<br />
deformation does not affect the 1:1000 scaled map. However, it will affect the <br />
<br />
<br />
<br />
position (coordinate) of the sorounding Geodesy Control Network (GCN). So, the <br />
<br />
<br />
<br />
GCN coordinates must be updated. |
---|