Carbonate deposition in the Central Luconia province initiated during the Early Miocene but was most profound during the Middle to Late Miocene. Although extensive regional studies have been completed by exploration and production (E&P) companies for decades, little has been published about the growth and demise of individual isolated carbonate platforms. Geological processes and the interaction between those processes are still poorly understood. Therefore, this research is conducted on the AX platform located in northwest of Central Luconia. The objectives of this study are to investigate key factors controlling the architecture of the isolated carbonate platform, to predict depositional environments and to predict facies distribution usi...
Karst is a common phenomenon in carbonate which was distributed widely in the Central Luconia carbo...
The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in a...
Modern Holocene carbonates are demonstrated to consist of distributions of their respective carbona...
During the Miocene, the Central Luconia Province offshore Sarawak became an area of carbonate produc...
During the Oligocene to Miocene, Southeast Asia was an equatorial region characterized by widespread...
Using 3D seismic reflection data and wireline logs we reconstruct in detail the architecture and gro...
The advances in karsts have revolved on the studies of onshore outcrops, high-resolution multi-beam ...
The Central Luconia province in the offshore NW Sarawak is a stable platform, flanked by two areas o...
This study is focused on an integrated geological analysis of both onshore and offshore Cenozoic ca...
The variability in low to moderate energy carbonate platform margins is poorly known from the geolog...
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. I...
Miocene carbonates have been studied on Palawan (Philippines), and compared to coeval deposits offsh...
Carbonate depositions can be found widely throughout the Central Luconia Province, but the identific...
Recently acquired 3-D seismic reflection data, wireline logs and selected core samples were used to ...
The Sanga Sanga PSC in the Kutai Basin of East Kalimantan is host to several gas and oil fields with...
Karst is a common phenomenon in carbonate which was distributed widely in the Central Luconia carbo...
The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in a...
Modern Holocene carbonates are demonstrated to consist of distributions of their respective carbona...
During the Miocene, the Central Luconia Province offshore Sarawak became an area of carbonate produc...
During the Oligocene to Miocene, Southeast Asia was an equatorial region characterized by widespread...
Using 3D seismic reflection data and wireline logs we reconstruct in detail the architecture and gro...
The advances in karsts have revolved on the studies of onshore outcrops, high-resolution multi-beam ...
The Central Luconia province in the offshore NW Sarawak is a stable platform, flanked by two areas o...
This study is focused on an integrated geological analysis of both onshore and offshore Cenozoic ca...
The variability in low to moderate energy carbonate platform margins is poorly known from the geolog...
Central Luconia is situated in the north of Bintulu in a water depth of approximately 40-160 feet. I...
Miocene carbonates have been studied on Palawan (Philippines), and compared to coeval deposits offsh...
Carbonate depositions can be found widely throughout the Central Luconia Province, but the identific...
Recently acquired 3-D seismic reflection data, wireline logs and selected core samples were used to ...
The Sanga Sanga PSC in the Kutai Basin of East Kalimantan is host to several gas and oil fields with...
Karst is a common phenomenon in carbonate which was distributed widely in the Central Luconia carbo...
The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in a...
Modern Holocene carbonates are demonstrated to consist of distributions of their respective carbona...