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- W2562485369 abstract "The D35 field is a sizeable hydrocarbon accumulation discovered by Shell in 1983, located 135 km north from Bintulu, within the Balingian Province of Offshore Sarawak. Hydrocarbons are contained within the stratigraphically complex Early to Middle Miocene clastic sediments, principally in Cycle II and to a lesser extent in the lower part of Cycle III. Its main hydrocarbon-bearing reservoirs comprise thick, stacked, cross-bedded sandstones, pebbly cross-bedded sandstones, sandy conglomerate and wavy-to-irregularly laminated sandstone. These sediments were initially interpreted by Shell as fluvial channel deposits, a model which was maintained until the relinquishment of the field in 2004." @default.
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- W2562485369 date "2008-01-01" @default.
- W2562485369 modified "2023-09-23" @default.
- W2562485369 title "The Evolution of Geological Thinking and Depositional Framework Interpretation through the Life of a Complex Reservoir, D35 Field, Offshore Sarawak" @default.
- W2562485369 doi "https://doi.org/10.3997/2214-4609-pdb.258.gl23" @default.
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