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- W197208643 abstract "Salt is found in three alternative structural settings in the southwestern Barents Sea region: (1) as domes and pillows in the platform areas, (2) as pillows, stocks and walls in some basins, and (3) as pillows along some graben margins. In the Nordkapp Basin there is clear evidence that halokinesis has interacted with faulting during structuring of the graben margins. Furthermore, periods with salt pillow growth are associated with condensed sedimentary sequences in the footwalls and expanded sequences in the hanging walls relative to the deep faults with which the pillows are associated. In general, this suggests flow of salt towards the basin margins. Some salt pillows are divided into subparallel elongated structures where they overlie deep faults. The crestal parts of the salt pillows are frequently faulted, and in some cases characterized by reverse fault geometries. The following sequence of events is proposed to explain this configuration: (1) salt flow directed towards basin margins; (2) continued deep faulting below the salt pillows associated with continued basin subsidence and basinward rotation of the basin margin areas; and (3) reactivation of crestal faults under differential compaction." @default.
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- W197208643 date "1992-01-01" @default.
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- W197208643 title "Interaction between halokinesis and faulting: structuring of the margins of the Nordkapp Basin, Barents Sea region" @default.
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- W197208643 doi "https://doi.org/10.1016/b978-0-444-88607-1.50013-9" @default.
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