Hostname: page-component-586b7cd67f-rdxmf Total loading time: 0 Render date: 2024-11-25T04:57:42.287Z Has data issue: false hasContentIssue false
  • English
  • Français

Reservoir quality and its relationship to facies and provenance in Middle to Upper Jurassic sequences, northeastern North Sea

Published online by Cambridge University Press:  09 July 2018

M. Ramm
M. Ramm*
Affiliation:
Norsk Hydro ASA, Exploration and Production, N-0246 Oslo, Norway
*
*E-mail: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

Close relationships are demonstrated between reservoir quality, lithofacies, provenance and burial history in the Jurassic Brent and Viking Groups in the Norwegian North Sea. Porosity and permeability are strongly and systematically related to the initial texture and composition of the sandstones. Porosity variations are related to the amount of compaction, which is more severe in matrix-rich than in clean facies, and quartz cementation, which is most important in clean facies. Permeability variations are related to porosity and facies-controlled variations in grain size, and abundance and texture of intergranular fines. Illitization of early diagenetic kaolins require K, which is derived mainly from dissolution of K-feldspar. Sediments were sourced from K-feldspar- poor provenances during the maximum progradation of the Brent Group, and sandstones deposited at this time are less exposed to illitization and have better permeability at deep burial than reservoir sandstones that initially contained more K-feldspar.

Keywords

reservoir qualityJurassic sequencesNorth Sea
Type
Research Article
Information
Clay Minerals , Volume 35 , Issue 1 , March 2000 , pp. 77 - 94
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bjørlykke, K. (1980) Clastic diagenesis and basin evolution. Rev. Inst. Geologias, Dep. Prov. Univ. Barcelona, 34, 34–21.Google Scholar
Bjørlykke, K., Aagaard, P., Dypvik, H., Hastings, D.S. & Harper, A.S. (1986) Diagenesis and reservoir properties of Jurassic sandstones from the Haltenbanken area, Offshore Mid Norway. Pp. 275-386 in: Habitat of Hydrocarbons on the Norwegian Continental Shelf (Spencer, A.M. et al, editors). Norwegian Petroleum Society, Graham & Trotman, London.Google Scholar
Bjørlykke, K., Ramm, M. & Saigal, G.C. (1989) Sandstone diagenesis and porosity modification during basin evolution. Geol. Runds. 78, 78–243.Google Scholar
Bjørlykke, K., Nedkvitne, T., Ramm, M. & Saigal, G.C. (1992) Diagenetic processes in the Brent Group (Middle Jurassic) reservoirs of the North Sea–an overview. Pp. 265-289 in. Geology of the Brent Group (Morton, A.C., Hazeldine, R.S., Giles, M.R. & Brown, S., editors). Geological Society London, Spec. Publ., 61, 61–265.Google Scholar
Ehrenberg, S.N. (1990) Relationship between diagenesis and reservoir quality in sandstones of the Gam Formation, Haltenbanken, Mid-Norwegian Continental Shelf. Am. Assoc. Petrol. Geol. Bull. 74, 74–1538.Google Scholar
Ehrenberg, S.N. (1993) Preservation of anomalous high porosity in deeply buried sandstones by graincoating chlorite: Examples from the Norwegian continental shel. Am. Assoc. Petrol. Geol. Bull. 77, 77–1260.Google Scholar
Ehrenberg, S.N. & Boassen, T. (1993) Factors controlling permeability variations in the sandstones of the Gam Formation in Trestakk Field, Norwegian Continental Shelf. J. Sed. Pet. 63, 63–929.Google Scholar
Ehrenberg, S.N. & Nadeau, P.H. (1989) Formation of diagenetic illite in sandstones of the Gam Formation, Haltenbanken area, Mid-Norwegian continental shelf. Clay Miner. 24, 24–233.CrossRefGoogle Scholar
Flesche, H., Nielsen, A.A., Larsen, R., Rykkje, J.M. & Ramm, M. (1998) Automatic classification of minerals from SEM EDS images, Mineralogical Society Winter Meeting: Microbeam Techniques in the Geosciences. (Abstract)Google Scholar
Fjellanger, E., Olsen, T.R & Rupino, J.L. (1996) Sequence stratigraphy and paleogeography of the Middle Jurassic Brent and Vestland deltaic systems, Northern North Sea. Norsk Geologisk Tidsskrift, 76, 76–75.Google Scholar
Giles, M.R., Stevenson, S., Martin, S.V., Cannon, S.J.C., Hamilton, P.J., Marshall, J.D. & Samways, G.M. (1992) The reservoir properties and diagenesis of the Brent Group: a regional perspective. Pp. 289-327 in: Geology of the Brent Group (Morton, A.C., Hazeldine, R.S., Giles, M.R. & Brown, S., editors). Geological Society London, Spec. Publ. 61.Google Scholar
Karstang, T.V., (1992) Multivariate calibration and prediction in the presence of background constituents : applications to spectroscopic data. PhD thesis, Univ. Bergen, Norway.Google Scholar
Johannesen, E.P., Mjøs, R., Renslaw, D., Dalland, A. & Jacobsen, T. (1995) Northern limit of the ‘Brent Delta’ at Tampen Spur–a sequence stratigraphie approach for sandstone prediction. Pp. 213-256 in: Sequence Stratigraphy on the Northwest European Margin (Steel, R.J., Felt, V., Johannesen, E.P. & Mathieu, C., editors). Norwegian Petroleum Society, Spec. Publ. 5.Google Scholar
Midtbø, R.E., Rykkje, J.M. & Ramm, M. (2000) Deep burial diagenesis and reservoir quality along the eastern flank of the Viking Graben. Evidence for illitization and quartz cementation after hydrocarbon emplacement. Clay Miner. 35, 35–227.Google Scholar
Morton, A.C, Hazeldine, R.S., Giles, M.C. & Brown, S. (1992) Geology of the Brent Group. Geological Society London., Spec. Publ., 61.Google Scholar
Ramm, M. (1992) Porosity depth trends in reservoir sandstones; Theoretical models related to Jurassic sandstones offshore Norway. Marine Petrol. Geol. 9, 9–553.Google Scholar
Ramm, M. & Bjørlykke, K. (1994) Porosity-depth trends in reservoir sandstones: Assessing the importance of mineralogy, pore-pressure and temperature from empirical data from the Norwegian Continental Shelf. Clay Miner. 29, 29–475.Google Scholar
Ramm, M. & Ryseth, A.E. (1996) Reservoir quality and burial diagenesis in the Statfjord Formation, North Sea. Petrol. Geosci. 2, 2–313.Google Scholar
Ramm, M., Forsberg, A.W. & Jahren, J.S. (1997) Porosity-depth trends in deeply buried Upper Jurassic reservoirs in the Norwegian Central Graben: An example of porosity preservation beneath the normal economic basement by graincoating microquartz. Pp. 177-199 in. Reservoir Quality Prediction in Sandstone and Carbonates (Kupecz, J.A., Gluyas, J. & Bloch, S., editors). Am. Assoc. Petrol. Geol. Memoir, 69, 69–177.Google Scholar