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- W3203523653 abstract "Summary A new paleogeographic model for the Late Paleocene to Early Eocene T40-T45 sequences ( Ebdon et al., 1995 chronostratigraphic nomenclature) for the Flett Sub-Basin (West of Shetlands Basin) has been constructed. Seismic interpretation (on 2D and 3D data) was integrated with wells information to constrain the spatial extension of the different gross depositional environments. During this period, the Flett Sub-Basin was semi-confined between the West of Shetland platform and the massive Faroe basalt plateau. A continental clastic wedge was deposited in the south west of the sub-basin whereas in the north east (at Bunnehaven and Tobbermory well location), starved deepwater settings prevailed. The basin was also marked by a multi-scale interaction of sedimentation with volcanism linked with the opening of the North Atlantic Ocean and the activity of the proto Icelandic mantle plume. Different scenario regarding sand paths (from the coastal domain to the deepwater basin) have been investigated. Despite all the efforts, no scenario prevailed on the others and Bunnehaven sands’ provenance remains ambiguous." @default.
- W3203523653 created "2021-10-11" @default.
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- W3203523653 date "2021-01-01" @default.
- W3203523653 modified "2023-10-16" @default.
- W3203523653 title "Rejuvenation of the T40-T45 paleogeography model in the Flett Sub-Basin (West of Shetlands)" @default.
- W3203523653 doi "https://doi.org/10.3997/2214-4609.202113334" @default.
- W3203523653 hasPublicationYear "2021" @default.
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