Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-27T06:45:07.506Z Has data issue: false hasContentIssue false

Fluid flow in the northern Broad Fourteens Basin during Late Cretaceous inversion

Published online by Cambridge University Press:  01 April 2016

L. Bouw*
Affiliation:
Delft University of Technology, Hydrology & Ecology Group, P.O. box 5048, 2600 GA Delft, the Netherlands
G.H.P. Oude Essink
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, P.O. box 80015, 3508TA Utrecht, the Netherlands (e-mail: g.oudeessink@nitg.tno.nl) & Vrije Universiteit Amsterdam, Faculty of Earth and Life Sciences, De Boelelaan 1085, 1081 HV Amsterdam, the Netherlands, e-mail: oudg@geo.vu.nl
*
1Corresponding author, e-mail: L.Bouw@CiTG.TUDelft.nl

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

A basin-scale hydrogeological study of the inverted northern Broad Fourteens Basin, Netherlands offshore, has resulted in a reconstruction of geological evolution, an estimate of Late Cretaceous topography and model scenarios of syn-inversion meteoric water infiltration. This study was performed in the scope of a basin-scale analysis of the hydrogeological setting and hydrodynamic evolution of the Broad Fourteens Basin. This analysis is aimed at obtaining quantitative knowledge of depositional history and hydrogeological parameters, and qualitative knowledge of hydrodynamic evolution of the Broad Fourteens Basin from Carboniferous to present-day. We present an overview of the tectonic and depositional history, the most likely hydrogeological setting and model scenarios of Late Cretaceous meteoric water infiltration in the northern Broad Fourteens area.

We constructed a detailed south-west north-east geological cross-section of the present-day northern Broad Fourteens Basin, and reconstructed Late Cretaceous basin geometry and topography. Using this geometry in a numerical model of density-dependent topography-driven fluid flow, we modelled several scenarios of meteoric water infiltration with estimated ranges of basin-scale permeabilities and water table head. Results indicate that a deep freshwater lens was developed during Late Cretaceous inversion, if the basin-scale hydraulic conductivity of the Rijnland and Altena Groups was at least 1⋅10-9 to 1⋅10-10 m/s, which is in general the highest value for claystones.

Type
Research Article
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2003

References

Beekman, H.E., Glasbergen, P., Slot, A.F.M. & Prins, H.F., 1989. Inventarisatie en evaluatie van geohydrologische gegevens van Noordoost en Oost Nederland ten behoeve van het onderzoek naar de opberging van radioactief afval in zoutformaties. RIVM (Bilthoven, the Netherlands): 242 pp.Google Scholar
Bjørlykke, K. & Gran, K., 1994. Salinity variations in North Sea formation waters: implications for large-scale fluid movements. Marine and Petroleum Geology 11: 59.CrossRefGoogle Scholar
Bouw, L., 1999. Geology, hydrogeology and hydrodynamics of the northern Broad Fourteens Basin, southern North Sea: a conceptual model. M. Sc. thesis, Department of Earth Sciences, Utrecht University & Netherlands Institute of Applied Geoscience TNO - National Geological Survey (Utrecht, the Netherlands): 160 pp.Google Scholar
Cornford, C. 1994. Mandal-Ekofisk (!) Petroleum system in the Central Graben of the North Sea. In: Magoon, L.B. & Dow, W.G. (eds): The petroleum system - from source to trap. AAPG Memoir 60: 537571.Google Scholar
De Marsily, G., 1986. Quantitative Hydrogeology. Groundwater hydrology for Engineers. Academic Press, Inc. (Orlando, Florida): 440 pp.Google Scholar
Dronkers, A.J. & Mrozek, F.J., 1991. Inverted basins of the Netherlands. First Break 9: 409425.CrossRefGoogle Scholar
Einsele, G., 1992. Sedimentary basins: evolution, facies and sediment budget. Springer-Verlag (Berlin, Germany): 628 pp.CrossRefGoogle Scholar
Gelhar, L.W., Welty, C. & Rehfeldt, K.R., 1992. A critical review of data on field-scale dispersion in aquifers. Water Resources Research 28: 19551974.CrossRefGoogle Scholar
Harbaugh, A.W. & McDonald, M.G., 1996. User’s documentation for the U.S.G.S. modular finite-difference ground-water flow model. U.S.G.S. Open-File Report 96-485: 56 pp.Google Scholar
Huyghe, P. & Mugnier, J.-L., 1994. Intra-plate stresses and basin inversion: A case from the Southern North Sea. In: Roure, F. (ed.): Peri-Tethyan Platforms. Edition Technip (Paris, France): 211226.Google Scholar
Huyghe, P. & Mugnier, J.-L., 1995. A comparison of inverted basins of the Southern North Sea and inverted structures of the external Alps. In: Buchanan, J.G. & Buchanan, P.G. (eds): Basic Inversion. Geological Society Special Publication 88: 339353.Google Scholar
Knott, S.D., 1993. Fault seal analysis in the North Sea. AAPG Bulletin 77: 778792.Google Scholar
Konikow, L.F., Goode, D.J. & Hornberger, G.Z., 1996. A three-dimensional method-of-characteristics solute-transport model (MOC3D). U.S.G.S.Water-Resources Investigations Report 96-4267: 87 pp.Google Scholar
Lee, M., Aronson, J.L., & Savin, S.M., 1989. Timing and conditions of Permian Rotliegende sandstone diagenesis, southern North Sea: K/Ar and oxygen isotopie data. AAPG Bulletin 73: 195215.Google Scholar
McDonald, M.G. & Harbraugh, A.W., 1988. A modular three-dimensional finite difference groundwater flow model. U.S.G.S. Techniques of Water-Resources Investigations, Book 6, Chapter Al, 586 pp.Google Scholar
Nalpas, Th., Le Douaran, S., Brun, J.-P., Unternehr, P. & Richert, J.-P., 1995. Inversion of the Broad Fourteens Basin (offshore Netherlands), a small-scale model investigation. Sedimentary Geology 95: 237250.CrossRefGoogle Scholar
Nalpas, Th., Riehen, J.-P., Mulder, T. & Unternehr, P., 1996. Inversion du ‘Broad Fourteens Basin’ ou Graben de la Haye (sud de la mer du Nord) - Apports de la sismique 3D. Bulletin des Centres Recherches Exploration-Production Elf Aquitaine 20: 309321.Google Scholar
Nopec, , 1988. North Sea Atlas, A structural encyclopaedia. Seismic atlas 3: section 91.Google Scholar
Oude Essink, G.H.P., 1999. Simulating 3D density-dependent groundwater flow: the adapted MOC3D. In: De Breuck, W. & Walschot, L (eds): Proceedings of the 15th Salt Water Intrusion Meeting. Natuur- en Geneeskundig Vennootschap (Ghent, Belgium): 6979.Google Scholar
Oude Essink, G.H.P., 2001. Salt water intrusion in a three-dimensional groundwater system in the Netherlands: A numerical study. Transport in Porous Media 43: 137158.CrossRefGoogle Scholar
Price, M., 1987. Fluid flow in the Chalk of England. In: Goff, J.C. & Williams, B.P.J. (eds): Fluid flow in sedimentary basins and aquifers. Geological Society Special Publication 34: 141156.Google Scholar
Purvis, K. & Okkerman, J.A., 1996. Inversion of reservoir quality by early diagenesis: an example from the Triassic Buntsandstein, offshore the Netherlands. In: Rondeel, H.E., Batjes, D.A.J. & Nieuwenhuijs, W.H. (eds): Geology of gas and oil under the Netherlands. Kluwer Academic Publishers (Dordrecht, the Netherlands): 179189.CrossRefGoogle Scholar
Remmelts, G., 1996. Salt tectonics in the southern North Sea, the Netherlands. In: Rondeel, H.E., Batjes, D.A.J. & Nieuwenhuijs, W.H. (eds): Geology of gas and oil under the Netherlands. Kluwer Academic Publishers (Dordrecht, the Netherlands): 143158.CrossRefGoogle Scholar
Roelofsen, J.W. & De Boer, W.D., 1991. Geology of the Lower Cretaceous Q/l oil-fields, Broad Fourteen Basin, The Netherlands. In: Spencer, A.M. (ed.): Generation, accumulation and production of Europe’s hydrocarbons. Special Publication of the European Association of Petroleum Geoscientists 1. Oxford University Press (Oxford, United Kingdom): 203216.Google Scholar
Roos, B.M. & Smits, B.J., 1983. Rotliegend and Main Buntsandstein gas fields in Block K/13 - A case history. Geologie en Mijnbouw 62: 7582.Google Scholar
Spain, D.R. & Conrad, P.C., 1997. Quantitative analysis of top-seal capacity: offshore Netherlands, southern North Sea. Geologie en Mijnbouw 76: 217226.CrossRefGoogle Scholar
Sullivan, M.D., Haszeldine, R.S., Boyce, A.J., Rogers, G. & Fallick, A.E., 1994. Late anhydrite cements mark basin inversion: isotopie and formation water evidence, Rotliegend Sandstone, North Sea. Marine and Petroleum Geology 11: 4654.CrossRefGoogle Scholar
Tóth, J., 1995. Hydraulic continuity in large sedimentary basins. Hydrogeology Journal 3: 416.CrossRefGoogle Scholar
Van Adrichem Boogaert, H.A. & Kouwe, W.F.P., 1993-1997. Stratigraphie nomenclature of the Netherlands, revision and update by RGD and NOGEPA. Mededelingen Rijks Geologische Dienst 50.Google Scholar
Van Wijhe, D.H., 1987a. The structural evolution of the Broad Fourteens Basin. In: Brooks, J. & Glennie, K.W. (eds) : Petroleum Geology of north west Europe. Graham and Trotman (London, United Kingdom): 315323.Google Scholar
Van Wijhe, D.H., 1987b. Structural evolution of inverted basins in the Dutch offshore. Tectonophysics 137: 171219.CrossRefGoogle Scholar
Verweij, J.M., 1999. Application of fluid flow systems analysis to reconstruct the post-Carboniferous hydrogeohistory of the onshore and offshore Netherlands. Marine and Petroleum Geology 16:561579.CrossRefGoogle Scholar
Verweij, J.M. & Simmelink, H.J., 2002. Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin (The Netherlands) in relation to its petroleum systems. Marine and Petroleum Geology 19: 339359 CrossRefGoogle Scholar
Verweij, J.M., Simmelink, H.J., David, P., Van Balen, R.T., Van Bergen, F. & Van Wees, J.D.A.M., 2000. Geodynamic and hydrodynamic evolution of the Broad Fourteens Basin and the development of its petroleum systems: an integrated 2D basin modelling approach. Journal of Geochemical Exploration 69-70: 635639.CrossRefGoogle Scholar
Warren, E.A. & Smalley, P.C., 1993. The chemical composition of North Sea formation waters: a review of heterogeneity and potential applications. In: Parker, J.R. (ed.): Petroleum Geology of Northwest Europe: Proceedings of the 4th conference. The Geological Society (London, United Kingdom): 13471352.Google Scholar