RESERVOIR CHARACTERIZATION OF PEMATANG 6200 AND MENGGALA 5900 OF BARUMUN SUB-BASIN USING INTEGRATION OF SEISMIC ATTRIBUTE ANALYSIS AND SPECTRAL DECOMPOSITION
Barumun sub basin is the northernmost sub basin in Central Suamtera Basin. High resolution 3D Seismic data which was acquired in 2003 and new exploratory well data in the 3D seismic area very useful to understand depositional system in Barumun sub basin. The objectives of this research are to und...
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Format: | Theses |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/70757 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Barumun sub basin is the northernmost sub basin in Central Suamtera Basin. High
resolution 3D Seismic data which was acquired in 2003 and new exploratory well
data in the 3D seismic area very useful to understand depositional system in
Barumun sub basin. The objectives of this research are to understand depositional
system, facies distribution and understanding reservoir characterization thin layer
sand in upper Pematang group and lower Sihapas group.
The main methodology in this research is using information from normal
amplitude of 3D seismic data, also using seismic attribute extraction and spectral
decomposition to view development geometry patterns in Barumun sub basin.
Those results were cross correlated each other to interpret comprehensively to
understand depositional environment and tracking thin bed layer. The existing
well data was used to validate the result.
The research’s results show that the integration between seismic attributes and
spectral decomposition successful to characterize thin bed reservoir in Pematang
6200 Formation and Menggala 5900 Formation. Pematang 6200 is dominated by
fluvial depositional of braided meandering stream, while Menggala 5900 is
depositional transition of marine and non marine with fluvial depositional of
meandering, estuarine and delta. This contrast depositional environment from
Pematang to Menggala from non marine to marine indicates tectonic regional
change. |
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