Add to ORKGMiocene Carbonate reservoirs located in Central Luconia Province, offshore NW Borneo. The interaction of eustatic sea level and basinal tectonics has a significant impact on the evolution of the build-ups. The Cycles I to VIII were born based on the repetitive nature of the sea level changes
Typically, the geology and production behavior of gas reservoirs in the atoll shaped Miocene carbona...
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. I...
More than 250 build-ups discovered within the Luconia Province, Offshore Sarawak
During the Oligocene to Miocene, Southeast Asia was an equatorial region characterized by widespread...
The porosity-permeability architecture of carbonate buildups in Central Luconia, Malaysia still rem...
During the Miocene, the Central Luconia Province offshore Sarawak became an area of carbonate produc...
International audienceUsing 3D seismic and well data, detailed seismic interpretation has been condu...
The Central Luconia province in the offshore NW Sarawak is a stable platform, flanked by two areas o...
Miocene carbonate reservoirs located in Central Luconia Province, offshore NW Borneo and Warrlich e...
Karst is a common phenomenon in carbonate which was distributed widely in the Central Luconia carbo...
The calibrated 3D seismic data were studied to characterize the carbonate facies in a carbonate bui...
The calibrated 3D seismic data were studied to characterize the carbonate facies in a carbonate bui...
The advances in karsts have revolved on the studies of onshore outcrops, high-resolution multi-beam ...
Using 3D seismic reflection data and wireline logs we reconstruct in detail the architecture and gro...
Carbonate deposition in the Central Luconia province initiated during the Early Miocene but was most...
Typically, the geology and production behavior of gas reservoirs in the atoll shaped Miocene carbona...
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. I...
More than 250 build-ups discovered within the Luconia Province, Offshore Sarawak
During the Oligocene to Miocene, Southeast Asia was an equatorial region characterized by widespread...
The porosity-permeability architecture of carbonate buildups in Central Luconia, Malaysia still rem...
During the Miocene, the Central Luconia Province offshore Sarawak became an area of carbonate produc...
International audienceUsing 3D seismic and well data, detailed seismic interpretation has been condu...
The Central Luconia province in the offshore NW Sarawak is a stable platform, flanked by two areas o...
Miocene carbonate reservoirs located in Central Luconia Province, offshore NW Borneo and Warrlich e...
Karst is a common phenomenon in carbonate which was distributed widely in the Central Luconia carbo...
The calibrated 3D seismic data were studied to characterize the carbonate facies in a carbonate bui...
The calibrated 3D seismic data were studied to characterize the carbonate facies in a carbonate bui...
The advances in karsts have revolved on the studies of onshore outcrops, high-resolution multi-beam ...
Using 3D seismic reflection data and wireline logs we reconstruct in detail the architecture and gro...
Carbonate deposition in the Central Luconia province initiated during the Early Miocene but was most...
Typically, the geology and production behavior of gas reservoirs in the atoll shaped Miocene carbona...
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. I...
More than 250 build-ups discovered within the Luconia Province, Offshore Sarawak