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Barumun Tengah Field is located in Central Sumatra Basin, North Sumatra. The field is a newly developed field since discovered with BT-1 well at 1984. Newly taken well and 3D seismic data at 2009-2011 shows several potential structures outside the developed structure. Distribution of depositional en...
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id-itb.:166482017-09-27T14:38:37Z#TITLE_ALTERNATIVE# NATASIA, NANDA Geologi, hidrologi & meteorologi Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/16648 Barumun Tengah Field is located in Central Sumatra Basin, North Sumatra. The field is a newly developed field since discovered with BT-1 well at 1984. Newly taken well and 3D seismic data at 2009-2011 shows several potential structures outside the developed structure. Distribution of depositional environment of Resrvoir 'A' of Menggala Formation interpreted from core and RMS amplitude attribute consist of seven genetic unit. They are open marine, barier bar, lagunal, tidal flat (sand flat, mixed flat, and mud flat) and supra tidal that deposited along Lagoon environment. Lateral distribution of tidal channel, sand flat, and lagoonal mud are at Northward to Center, and barier bar are at Southern area with Northwest – Southeast trending. There are three potential structure could be fund that barier bar facies. The three prospect are in medium to high quality based on the distribution of net sand reserfoir and porosity (14 -20% porosity). Highest potential is at Prospect 1 with reserve calculation are: P10 2,04 MMSTB; P50 9,2 MMSTB; and P90 22,6 MMSTB. text |
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Geologi, hidrologi & meteorologi NATASIA, NANDA #TITLE_ALTERNATIVE# |
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Barumun Tengah Field is located in Central Sumatra Basin, North Sumatra. The field is a newly developed field since discovered with BT-1 well at 1984. Newly taken well and 3D seismic data at 2009-2011 shows several potential structures outside the developed structure. Distribution of depositional environment of Resrvoir 'A' of Menggala Formation interpreted from core and RMS amplitude attribute consist of seven genetic unit. They are open marine, barier bar, lagunal, tidal flat (sand flat, mixed flat, and mud flat) and supra tidal that deposited along Lagoon environment. Lateral distribution of tidal channel, sand flat, and lagoonal mud are at Northward to Center, and barier bar are at Southern area with Northwest – Southeast trending. There are three potential structure could be fund that barier bar facies. The three prospect are in medium to high quality based on the distribution of net sand reserfoir and porosity (14 -20% porosity). Highest potential is at Prospect 1 with reserve calculation are: P10 2,04 MMSTB; P50 9,2 MMSTB; and P90 22,6 MMSTB. |
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