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- W2296968895 abstract "A series of regionally correlatable unconformity bounded sequences has been identified within the Paleocene interval of the West of Shetland area. These sequences contain a succession of sandstones deposited in deep-water environments within the Early to ‘mid’ Paleocene (Danian to early Thanetian) with a gradual shallowing upwards to shelf and deltaic deposits in the Late Paleocene. Reservoir properties of these sandstones vary widely, with porosities ranging from >30% to below 10%, and permeabilities from >2D to 20%) and permeabilities (10–100 mD) at below 3 km burial depth. This preservation of reservoir quality is due in part to depositional facies, but mineralogical/diagenetic variability has also allowed the preservation of porosity and permeability. In particular, the presence of grain rimming chlorite in these sandstones is fundamental in preserving porosity. Log and core analyses of these sandstones has shown that interpretation of reservoir potential and fluid saturations is not straightforward. The effect of diagenetic minerals on log responses and in particular the salinity of formation waters (both in water- and hydrocarbon-bearing zones) were poorly known at the start of the study, and had to be accurately quantified. The integration of all available data, including intensive study of core material, allowed the definition of these effects and thus allowed the adequate modelling of hydrocarbon saturations." @default.
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- W2296968895 date "1999-01-01" @default.
- W2296968895 modified "2023-09-28" @default.
- W2296968895 title "Reservoir quality and petrophysical evaluation of Paleocene sandstones in the West of Shetland area" @default.
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- W2296968895 doi "https://doi.org/10.1144/0050627" @default.
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