1887

Abstract

B-27 RESERVOIR CHARACTERIZATION OF THE GRANE FIELD WITH MULTI-COMPONENT SEISMIC DATA Introduction 1 The Grane Field is located at the eastern margin of the Viking Graben on the western flank of the Utsira high. The Grane Field consists of Palaeocene turbidite sandstones (Heimdal Formation) which originate from the East Shetland Platform to the West of the field. The deposition and geometry of the turbidite sand lobes were mostly controlled by the original basin morphology which forced the sand to deposit along a main N-S axis parallel to the Utsira High. The Heimdal Fm consists of high-density turbidite sandstones that were

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/content/papers/10.3997/2214-4609-pdb.6.B27
2003-06-02
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.6.B27
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