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Petroleum Geoscience; May 2006; v. 12; no. 2; p. 175-190; DOI: 10.1144/1354-079305-693
© 2006 Geological Society of London
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Original Article

Contribution of research borehole data to modelling fine-grained turbidite reservoir analogues, Permian Tanqua–Karoo basin-floor fans (South Africa)

Stefan M. Luthi1, David M. Hodgson2, Cees R. Geel1,3, Stephen S. Flint2, Jan Willem Goedbloed1,5, Nicholas J. Drinkwater4 and Erik P. Johannessen5

1 Department of Geotechnology, Delft University of Technology, Mijnbouwstraat 120, 2628 RX Delft, The Netherlands (e-mail: s.m.luthi@citg.tudelft.nl)
2 Stratigraphy Group, Department of Earth & Ocean Sciences, 4 Brownlow Street, Liverpool L69 3GP, UK
3 Present address: Netherlands Institute for Applied Geoscience TNO, Department of Geo-Energy, PO Box 80.015,3508 TA Utrecht, The Netherlands
4 Schlumberger Cambridge Research, High Cross, Madingley Road, Cambridge CB3 0EL, UK (Present address: Chevron Corporation, Energy Technology Company, 1500 Louisiana Street, Houston TX 77002, USA)
5 Statoil, Forushagen, Grenseveien 21, Stavanger, N-4035, Norway

Outcrop analogue studies can be augmented and constrained by drilling research wells through the same stratigraphic interval. Close-to-outcrop wells help to validate outcrop observations with well log and core data and thus improve the use of such data in actual field developments. Research wells located further away from the outcrops increase the spatial data coverage and can give important insight into regional facies distributions and net:gross changes.

In the Tanqua–Karoo Basin (South Africa), seven wells were drilled into fine-grained sand-rich basin-floor fans and interfan mudstones to supplement outcrop data. Three close-to-outcrop wells proved useful in establishing characteristic log responses of the main architectural elements identified from the nearby outcrops. Lithofacies were correctly identified in more than 80% of cases using an artificial neural network. Borehole images provided detailed information on sedimentary structures, including a wealth of palaeocurrent data from climbing ripples that significantly enhanced the interpretations based only on outcrops. Wells sited away from the outcrops supplied information on lateral thickness and facies trends and intrafan stacking patterns, which helped to define the stratigraphic evolution of the fans. The combined data indicate that deposition was controlled in part by subtle basin-floor topography, and that intrafan lobe switching took place, leading to internal subdivisions that potentially caused effective compartmentalization of the basin-floor fan.

KEYWORDS: outcrop studies, well data, basin-floor fans, Tanqua–Karoo Basin




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[Abstract] [Full Text] [PDF]




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