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Petroleum Geoscience; February 2008; v. 14; no. 1; p. 17-34; DOI: 10.1144/1354-079307-787
© 2008 Geological Society of London
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Original Article

Sedimentological parameterization of shallow-marine reservoirs

John A. Howell1,2, Arne Skorstad3, Alister MacDonald4, Alex Fordham2, Stephen Flint2, Bjørn Fjellvoll3 and Tom Manzocchi5

1 Department of Earth Science/Centre for Integrated Petroleum Research, University of Bergen, Allegt. N-5007 Bergen, Norway
2 Sequence Stratigraphy Group, Department of Earth and Ocean Sciences, University of Liverpool, Liverpool L69 3GP, UK
3 Norwegian Computing Center, PO Box 114 Blindern, N-0314 Oslo, Norway
4 Roxar Software Solutions, 165 Skoyen, Karenslyst Alle 11, 0212 Oslo, Norway
5 Fault Analysis Group, UCD School of Geological Sciences, University College Dublin, Belfield, Dublin, Ireland

The key causes of heterogeneity within progradational shallow-marine reservoirs have been defined as: shoreline type (wave vs. fluvial dominated); shoreline trajectory; the presence of permeability contrasts associated with dipping clinoform surfaces within the shoreface or delta front; the presence of cemented barriers between parasequences; and the progradation direction of the shoreline (described with respect to the main waterflood direction in the simulated reservoir). These parameters were recorded from a series of 56 modern and ancient depositional systems from a variety of climatic and tectonic settings. These data were then used to build the 408 synthetic sedimentological models that formed the basis for the SAIGUP study.

KEYWORDS: shoreface, delta, reservoir, modelling




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