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- W60061820 abstract "Abstract Applying one- and two-dimensional fluid-flow/compaction models to the NW part of the Danish Central Graben, the geohistory, thermal history, source capacity and oil generation were examined. The burial history shows that the NW Danish Central Graben developed through several stages of subsidence — a Late Jurassic differential stage, a Late Cretaceous/Early Tertiary uniform stage and a Late Miocene/Quaternary uniform stage. The thermal history is assessed by inversion of measured vitrinite reflectance with depth and all wells give a consistent cooler past; resolution of the available data on the thermal history is discussed. Pseudo-wells have been “drilled” on seismic sections in areas without well data. Synthetic vitrinite reflectance data have been generated for the pseudo-wells using the modelled thermal history. The sensitivity of the maturity and thermal history modelling to changes in parameters such as erosion events, errors in the present day heat flow and paleo-overpressure evolution is discussed. The modelled maturation history of the Late Jurassic shale shows that the shale reached maturity some 5–50 Ma. Modelling of the hydrocarbon generation indicates that the peak generation took place some time between 10 Ma and the present day. Possible migration paths are determined from modelled excess fluid pressure and areas of possible accumulation of hydrocarbons are indicated. The potentials of the areas are evaluated and an area along the eastern boundary fault between the Tail End Graben and the Ringkobing-Fyn High is suggested as a prospective new target for further exploration." @default.
- W60061820 created "2016-06-24" @default.
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- W60061820 date "1992-01-01" @default.
- W60061820 modified "2023-09-27" @default.
- W60061820 title "The Danish North Sea: a basin prognosis" @default.
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- W60061820 doi "https://doi.org/10.1016/b978-0-444-88607-1.50035-8" @default.
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