IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION

Oil and natural gas hydrocarbon are one of the most important natural resources in the era of technological advancement nowadays. The needs and demand for oil and natural gas is increasing. To fulfill this need, exploration is carried out in deep sewa waters. The Kutai Basin is included in deep w...

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Main Author: Putra Pratama, Vallen
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/54256
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:54256
spelling id-itb.:542562021-03-15T15:21:30ZIDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION Putra Pratama, Vallen Indonesia Final Project shallow geohazard, seismic attribute, seismic inversion, Kutai Basin INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/54256 Oil and natural gas hydrocarbon are one of the most important natural resources in the era of technological advancement nowadays. The needs and demand for oil and natural gas is increasing. To fulfill this need, exploration is carried out in deep sewa waters. The Kutai Basin is included in deep water exploration, because the Kutai Basin is the largest and deepest basin with the second largest hydrocarbon reserves in Indonesia. Identification of geological hazards or better known as geohazard is needed in oil and gas exploration activities in deep sea waters. The existence of shallow geohazard is very important in the strategic plan of developing new fields, and if it is not considered, it will cause great losses. Shallow geohazard in deep sea water explorations is different from on land. Identification of shallow geohazard starts from pleistocene to recent. To identify the presence of shallow geohazard in the study area, a stratigraphic anlysis of 3D PSTM seismic data and analysis of seismic attributes are carried out. The seismic attributes that used to identify the presence of shallow geohazard are cosine of instantaneous phase, variance reflection strength, azimuth, and edge detection/dip angle. The identified shallow geohazards in this area steep slope, carbonate build up, submarine canyon, eroded seabed, shallow fault, and mass transport complexes. An analysis of the potential shallow geohazard was carried out and the distribution map was made of each shallow geohazard in this area which was then obtained the drilling favorability map. 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 Oil and natural gas hydrocarbon are one of the most important natural resources in the era of technological advancement nowadays. The needs and demand for oil and natural gas is increasing. To fulfill this need, exploration is carried out in deep sewa waters. The Kutai Basin is included in deep water exploration, because the Kutai Basin is the largest and deepest basin with the second largest hydrocarbon reserves in Indonesia. Identification of geological hazards or better known as geohazard is needed in oil and gas exploration activities in deep sea waters. The existence of shallow geohazard is very important in the strategic plan of developing new fields, and if it is not considered, it will cause great losses. Shallow geohazard in deep sea water explorations is different from on land. Identification of shallow geohazard starts from pleistocene to recent. To identify the presence of shallow geohazard in the study area, a stratigraphic anlysis of 3D PSTM seismic data and analysis of seismic attributes are carried out. The seismic attributes that used to identify the presence of shallow geohazard are cosine of instantaneous phase, variance reflection strength, azimuth, and edge detection/dip angle. The identified shallow geohazards in this area steep slope, carbonate build up, submarine canyon, eroded seabed, shallow fault, and mass transport complexes. An analysis of the potential shallow geohazard was carried out and the distribution map was made of each shallow geohazard in this area which was then obtained the drilling favorability map.
format Final Project
author Putra Pratama, Vallen
spellingShingle Putra Pratama, Vallen
IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
author_facet Putra Pratama, Vallen
author_sort Putra Pratama, Vallen
title IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
title_short IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
title_full IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
title_fullStr IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
title_full_unstemmed IDENTIFICATION SHALLOW GEOHAZARD IN DEEP WATER REGION “VP” USING INTEGRATION ANALYSIS OF SEISMIC ATTRIBUTE AND SEISMIC INVERSION
title_sort identification shallow geohazard in deep water region “vp” using integration analysis of seismic attribute and seismic inversion
url https://digilib.itb.ac.id/gdl/view/54256
_version_ 1822001729674149888