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• W1575432835 abstract "The reservoir interval of the Ormen Lange Field (Møre Basin) consists of two units, a lower heterolithic unit mainly of Maastrichtian age (Jorsalfare Formation) and an upper sandstone unit of Danian age (Egga member, Vale Formation). The Cretaceous-Tertiary boundary is located in the uppermost part of the unit. The Egga member has long been known as a potentially prolific reservoir interval in the Slørebotn Subbasin area, where it is up to 150 m thick, consisting of thick, amalgamated medium- to coarse-grained sandstone turbidites. The base of the Egga member in the Slørebotn Subbasin and in other areas close to the eastern margin of the Møre Basin is a significant unconformity, with the Danian succession usually overlaying strata of Campanian age. This unconformity developed during Maastrichtian times with shelf erosion and sediment bypass. The bypassed coarse clastic sediments were redeposited as turbidites further out in the Møre Basin, and represent the lower, heterolithic reservoir unit in the Ormen Lange Field. In early Danian time uplift and rotation of the Fennoscandian provenance area in the east led to extensive erosion and redistribution of sandy sediments that prograded westwards into the Møre Basin and gave rise to amalgamated turbidites of the Egga member. These turbidites probably filled a shallow intraslope basin or depression in the Sløreboth Subbasin and laterally bypassed into the deeper part of the Møre Basin, where relatively thick turbidites accumulated to form the upper reservoir interval of the Ormen Lange Field. During latest Cretaceous and Palaeogene times the location of the Ormen Lange Field was an area of relatively rapid subsidence, probably with the development of a temporary basin floor depression where deep water sediments were deposited. Inversion and development of the Ormen Lange structure took place in latest Eocene-Early Oligocene time. A considerable change in mineralogy and ichnofabric occurs at the Cretaceous-Tertiary boundary, indicating significant changes in the depositional environment." @default.
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• W1575432835 date "2001-01-01" @default.
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• W1575432835 title "The maastrichtian and danian depositional setting, along the eastern margin of the Møre Basin (mid-norwegian shelf): implications for reservoir development of the Ormen Lange Field" @default.
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• W1575432835 doi "https://doi.org/10.1016/s0928-8937(01)80025-4" @default.
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