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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Main Author: AGATHA NATANIA (NIM: 12313058), KANA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/22749
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:22749
spelling 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
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 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
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