APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD
Muara Laboh geothermal field is located in South Solok Regency, 150 km from <br /> <br /> <br /> <br /> <br /> Padang city. This field has been explored since 2007 and estimated to have a <br /> <br /> <br /> <br /> <br /> capac...
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id-itb.:227492017-10-09T10:31:18ZAPPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD AGATHA NATANIA (NIM: 12313058), KANA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/22749 Muara Laboh geothermal field is located in South Solok Regency, 150 km from <br /> <br /> <br /> <br /> <br /> Padang city. This field has been explored since 2007 and estimated to have a <br /> <br /> <br /> <br /> <br /> capacity of 220 Mw. In this field there are 6 wells and several geophysical data <br /> <br /> <br /> <br /> <br /> acquisition such as microseismic and magnetotelluric method has been performed. <br /> <br /> <br /> <br /> <br /> The Muara Laboh geothermal field status is on exploration stage and requires <br /> <br /> <br /> <br /> <br /> further information to enter the exploitation stage. Therefore the author models <br /> <br /> <br /> <br /> <br /> the velocity structure under the Muara Laboh reservoir. This study uses 135 <br /> <br /> <br /> <br /> <br /> microearthquakes data from September 14, 2010 to April 2, 2011 and 2692 <br /> <br /> <br /> <br /> <br /> microearthquakes from September 23, 2012 to December 22, 2013 with a total of <br /> <br /> <br /> <br /> <br /> 2827. A microseismic earthquake was recorded on 32 scattered station networks. <br /> <br /> <br /> <br /> <br /> To maximize the result of picking waveform, the data is processed using the <br /> <br /> <br /> <br /> <br /> Master Event Cross Correlation method to update the catalog data and get more <br /> <br /> <br /> <br /> <br /> accurate results. Furthermore, the author used TomoDD software to produce <br /> <br /> <br /> <br /> <br /> hypocenter relocation and the 3D velocity structure under Muara Laboh's <br /> <br /> <br /> <br /> <br /> geothermal reservoir. The results of the 3D velocity model can be used to <br /> <br /> <br /> <br /> <br /> determine the structure and fluid phase under Muara Laboh geothermal field. text |
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Muara Laboh geothermal field is located in South Solok Regency, 150 km from <br />
<br />
<br />
<br />
<br />
Padang city. This field has been explored since 2007 and estimated to have a <br />
<br />
<br />
<br />
<br />
capacity of 220 Mw. In this field there are 6 wells and several geophysical data <br />
<br />
<br />
<br />
<br />
acquisition such as microseismic and magnetotelluric method has been performed. <br />
<br />
<br />
<br />
<br />
The Muara Laboh geothermal field status is on exploration stage and requires <br />
<br />
<br />
<br />
<br />
further information to enter the exploitation stage. Therefore the author models <br />
<br />
<br />
<br />
<br />
the velocity structure under the Muara Laboh reservoir. This study uses 135 <br />
<br />
<br />
<br />
<br />
microearthquakes data from September 14, 2010 to April 2, 2011 and 2692 <br />
<br />
<br />
<br />
<br />
microearthquakes from September 23, 2012 to December 22, 2013 with a total of <br />
<br />
<br />
<br />
<br />
2827. A microseismic earthquake was recorded on 32 scattered station networks. <br />
<br />
<br />
<br />
<br />
To maximize the result of picking waveform, the data is processed using the <br />
<br />
<br />
<br />
<br />
Master Event Cross Correlation method to update the catalog data and get more <br />
<br />
<br />
<br />
<br />
accurate results. Furthermore, the author used TomoDD software to produce <br />
<br />
<br />
<br />
<br />
hypocenter relocation and the 3D velocity structure under Muara Laboh's <br />
<br />
<br />
<br />
<br />
geothermal reservoir. The results of the 3D velocity model can be used to <br />
<br />
<br />
<br />
<br />
determine the structure and fluid phase under Muara Laboh geothermal field. |
format |
Final Project |
author |
AGATHA NATANIA (NIM: 12313058), KANA |
spellingShingle |
AGATHA NATANIA (NIM: 12313058), KANA APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
author_facet |
AGATHA NATANIA (NIM: 12313058), KANA |
author_sort |
AGATHA NATANIA (NIM: 12313058), KANA |
title |
APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
title_short |
APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
title_full |
APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
title_fullStr |
APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
title_full_unstemmed |
APPLICATION OF TOMOGRAPHY DOUBLE DIFFERENCE TO DETERMINE 3D VELOCITY MODEL IN MUARA LABOH GEOTHERMAL FIELD |
title_sort |
application of tomography double difference to determine 3d velocity model in muara laboh geothermal field |
url |
https://digilib.itb.ac.id/gdl/view/22749 |
_version_ |
1821120869142888448 |