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Effects of burial on the clay assemblages in the Triassic Skagerrak Formation, Denmark

Published online by Cambridge University Press:  09 July 2018

R. Weibel
R. Weibel*
Affiliation:
Department of Earth Sciences, University of Aarhus, 8000 Aarhus C, Denmark
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Abstract

Sandstones and mudstones of the Skagerrak Formation from the Danish Sub-basin have been studied to assess the origin of the clay minerals, their diagenesis and their transformation/ conversion temperatures (compared to modelled maximum burial temperatures). Detrital smectite and vermiculite occur only at shallow levels. Conversion of smectite into random S-I took place at >47°C and of random S-I into ordered I-S at >74°C. The omnipresent illite increases in amount with burial. The amount of authigenic kaolinite (kaolin) decreases with increasing temperature (>75°C), possibly due to the growth of chlorite. Random S-C is converted into ordered S-C between 70°C and 105°C and chlorite is most abundant at maximum burial temperatures (150°C). This investigation suggests that diagenesis of clay minerals begins at relatively low temperatures, and emphasizes the importance of the availability of necessary ions (K+, Mg2+, Fe2+) for the reactions, besides time and temperature, as controlling parameters.

Type
Research Article
Information
Clay Minerals , Volume 34 , Issue 4 , December 1999 , pp. 619 - 635
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1999

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References

Allen, J.R.L. (1974) Studies in fluviatile sedimentation: implication of pedogenic carbonate units, Lower Old Red Sandstone, Anglo-Welsh outcrop. Geol. J. 9, 181–208.Google Scholar
Balling, N., Nielsen, S.B., Christiansen, H.S., Christensen, L.D. & Poulsen, S. (1992) The subsurface thermal regime and temperature of geothermal reservoirs in Denmark. Synthesis report to Commission of the European Communities, Contract EN3G-0029-DK. Department of Earth Sciences, Geophysical Laboratory, University of Aarhus, Denmark.Google Scholar
Bartier, D., Buatier, M., Lopez, M., Potdevin, J.L., Chamley, H. & Arostegui, J. (1998) Lithological control on the occurrence of chlorite in the diagenetic Wealden complex of the Bilbao anticlinorium (Basco-Cantabrian Basin, Northern Spain). Clay Miner. 33, 317–332.Google Scholar
Beaufort, D., Cassagnabere, A., Petit, S., Lanson, B., Berger, G., Lacharpagne, J.C. & Johansen, H. (1998) Kaolinite-to-dickite reaction in sandstone reservoirs. Clay Miner. 33, 297–316.Google Scholar
Berner, R.A. (1969) Goethite stability and origin of red beds. Geochim. Cosmochim. Ada, 35, 267–273. Bertelsen, F. (1980) Lithostratigraphy and depositional history of the Danish Triassic. Geol. Surv. Denmark, B, 4.Google Scholar
Bjørlykke, K. & Aagaard, P. (1992) Clay minerals in North Sea sandstones. Pp. 65—80 in: Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones (Houseknecht, D.W. & Pittman, E.D., editors). SEPM, Special Publication, 47, Tulsa, Oklahoma.Google Scholar
Burley, S. (1984) Patterns of diagenesis in the Sherwood Sandstone Group (Triassic), United Kingdom. Clay Miner. 19, 403–440.Google Scholar
Chang, H., MacKenzie, F.T. & Schoonmaker, J. (1986) Comparisons between the diagenesis of dioctahedral and trioctahedral smectite, Brazilian offshore basins. Clays Clay Miner. 34, 407–423.Google Scholar
Colson, J., Cojan, I. & Thiry, M. (1998) A hydrogeological model for palygorskite formation in the Danian continental facies of the Provence Basin (France). Clay Miner. 33, 333–347.CrossRefGoogle Scholar
Curtis, C.D. (1983) Link between aluminium mobility and destruction of secondary porosity. Am. Assoc. Petrol. Geol. Bull. 67, 380–393.Google Scholar
Curtis, C.D., Hughes, C.R., Whiteman, J.A. & Whittle, C.K. (1985) Compositional variation within some sedimentary chlorites and some comments on their origin. Mineral. Mag. 49, 375–386.Google Scholar
Deegan, C.E. & Scull BJ. (1977) A standard lithostratigraphic nomenclature for the Central and Northern North Sea. Institute of Geological Sciences & Norwegian Petroleum Directorate (Oljedirektoratet), Report 77/25, Bull. 1. Google Scholar
Dowdle, W.L. & Cobb, W.M. (1975) Static formation temperature from well logs and empirical method. J. Petrol. Technol. 27, 1326–1330.Google Scholar
Ehrenberg, S.N., Aagaard, P., Wilson, M.J., Fraser, A.R. & Duthie, D.M.L. (1993) Depth-dependent transformation of kaolinite to dickite in sandstones of the Norwegian continental shelf. Clay Miner. 28, 325–352.Google Scholar
Eslinger, E. & Pevear, D. (1988) Clay Minerals for Petroleum Geologists and Engineers. SEPM short course notes, 22, Tulsa, Oklahoma.Google Scholar
Fine, S. (1986) The diagenesis of the Lower Triassic Bunter Sandstone Formation, Onshore Denmark. Geol. Survey of Denmark A, 15.Google Scholar
Fisher, M.J. & Mudge, D.C. (1990) Triassic. Pp. 191—218 in: Introduction to the Petroleum Geology of the North Sea, Third Edition (Glennie, K.W., editor). Blackwell Scientific Publications, Oxford.Google Scholar
Garrels, R.M. & Christ, C.L. (1965) Solutions, Minerals, and Equilibria. Harper & Row, New York, 352-378.Google Scholar
Grim, R.E. (1968) Clay Mineralogy, Second Edition, McGraw-Hill, Inc., New York.Google Scholar
Hillier, S. (1993) Origin, diagenesis, and mineralogy of chlorite minerals in Devonian lacustrine mudrocks, Orcadian Basin, Scotland. Clays Clay Miner., 41, 240–259.Google Scholar
Humphreys, B., Smith, S.A. & Strong, G.E. (1989) Authigenic chlorite in Late Triassic sandstones from the Central Graben, North Sea. Clay Miner. 24, 427–444.Google Scholar
Humphreys, B., Kemp, S.J., Lott, G.K., Bermanto, Dharmayanti, D.A. & Samsori, I. (1994) Origin of grain-coating chlorite by smectite transformation: an example from Miocene sandstones, North Sumatra back-arc basin, Indonesia. Clay Miner. 29, 681–692.Google Scholar
Hutcheon, I., Oldershaw, A. & Ghent, E.D. (1980) Diagenesis of Cretaceous sandstones of the Kootenay Formation at Elk Vally (southeastern British Columbia) and Mt Allan (southwestern Alberta). Geochim. Cosmochim. Ada, 44, 1425–1435.Google Scholar
Japsen, P. (1992) LandhEevningerne i Sen Kridt og Tertifer i det nordlige Danmark. Bull. Geol. Soc. Denmark, Arsskrift for 1990-91, 169–182.Google Scholar
Jeans, C.V. (1978) The origin of the Triassic clay assemblages of Europe with special reference to the Keuper Marl and Rhaetic of parts of England. Phil. Trans. R. Soc. Lond. 289, 549–639.Google Scholar
Jeans, C.V. (1995) Clay mineral stratigraphy in Palaeozoic and Mesozoic red bed facies onshore and offshore UK. Pp. 31 — 55 in: Non-biostratigraphical Methods of Dating and Correlation (Dunay, R.E. & Hailwood, E.A., editors), Geological Society Special Publication, 89, London.Google Scholar
Jensen, L.N. & Michelsen, O. (1992) Tertifer htevning og erosion i Skagerrak, Nordjylland og Kattegat. Bull. Geol. Soc. Denmark, Arsskrift for 1990-91, 159–168.Google Scholar
Keller, W.D., Reynolds, R.C. & Inoue, A. (1986) Morphology of clay minerals in smectite-to-illite conversion series by scanning electron microscopy. Clays Clay Miner., 34, 187–197.Google Scholar
Krauskopf, K.B. (1967) Introduction to Geochemistry. McGraw-Hill, Inc., New York.Google Scholar
Laier, T. (1989) Mapping of low enthalpy brines in Denmark for geothermal exploitation. Pp. 409—412 in: Water-Rock Interactions (Miles, D.L., editor). Balkema, Rotterdam.Google Scholar
Langmuir, D. (1971) Particle size effect on the reaction goethite = hematite + water. Am. J. Sci. 271, 147–156.Google Scholar
Larson, E.E. & Walker, T.R. (1975) Development of chemical remanent magnetization during early stages of red-bed formation in late Cenozoic sediments, Baja California. Geol. Soc. Am. Bull, 86, 639–650.Google Scholar
Liboriussen, J., Ashton, P. & Tygesen, T. (1987) The tectonic evolution of the Fennoscandian Border Zone in Denmark. Tectonophys. 137, 21–29.Google Scholar
MacEwan, D.M.C. & Wilson, M.J. (1980) Interlayer and intercalation complexes of clay minerals. Pp. 197—248 in: Crystal Structures of Clay Minerals and their X-ray Identification. (Brindley, G.W. & Brown, G., editors). Mineralogical Society, London.Google Scholar
Michelsen, O. & Nielsen, L.H. (1993) Structural development of the Fennoscandian Border Zone, offshore Denmark. Marine Petrol. Geol. 10, 124–134.Google Scholar
Mumme, W.G., Tsambourakis, G., Madsen, I.C, & Hill, R.J. (1996) Improved petrological modal analysis from X-ray powder diffraction data by the use of the Rietveld method. Part II. Selected sedimentary rocks. J. Sedim. Res. 66, 132–138.Google Scholar
Nielsen, L.H., Larsen, F. & Frandsen, N. (1989) Upper Triassic-Lower Jurassic tidal deposits of the Gassum Formation on Sjtelland, Denmark. Geol. Surv. Denmark, A, 23.Google Scholar
Nielsen, L.H. & Japsen, P. (1991) Deep wells in Denmark 1935-1990. Geol. Survey of Denmark A, 31.Google Scholar
Pearson, M.J. & Small, J.S. (1988) Illite-smectite diagenesis and palaeotemperatures in northern North Sea Quaternary to Mesozoic shale sequences. Clay Miner. 23, 109–139.Google Scholar
Pedersen, G.K. & Andersen, P.R. (1980) Depositional environments, diagenetic history and source areas of some Bunter Sandstones in northern Jutland. Geol. Surv. Denmark, Arbog 1979, 69–93.Google Scholar
Perry, E. & Hower, J. (1970) Burial diagenesis in Gulf Coast pelitic sediments. Clays Clay Miner. 18, 165–177.CrossRefGoogle Scholar
Platt, J.D. (1993) Controls on the clay mineral distribution and chemistry in the early Permian Rotliegend of Germany. Clay Miner. 28, 393–416.Google Scholar
Pollastro, R.M. (1985) Mineralogical and morphological evidence for the formation of illite at the expense of illite/smectite. Clays Clay Miner. 33, 265–274.Google Scholar
Pollastro, R.M. (1993) Considerations and applications of the illite/smectite geothermometer in hydrocarbon- bearing rocks of Miocene to Mississippian age. Clays Clay Miner. 41, 119–133.Google Scholar
Priisholm, S. (1983) Geothermal reservoir rocks in Denmark. Geol. Surv. Denmark, Arbog 1982, 73–86.Google Scholar
Ramberg, I.B. & SpjeldnEES, N. (1977) The tectonic history of the Oslo Region. Pp. 167-194 in: Tectonics and Geophysics of the Continental Rifts (Ramberg, I.B. & Neumann, E.R., editors). D. Reidel Publishing Company, Dordrecht, The Netherlands.Google Scholar
Ramseyer, K. & Boles, J.R. (1986) Mixed-layer illite/ smectite minerals in Tertiary sandstones and shales San Joaquin Basin, California. Clays Clay Miner. 34, 115–124.Google Scholar
Reynolds, R.C. (1980) Interstratified clay minerals. Pp. 249—303 in: Crystal Structures of Clay Minerals and their X-ray Identification. (Brindley, G.W. & Brown, G., editors). Mineralogical Society, London.Google Scholar
Slater, J.G. & Christie, P.A.F. (1980) Continental stretching: an explanation of the post-mid- Cretaceous subsidence of the Central North Sea Basin. J. Geophys. Res. 85, B7, 3711–3739.Google Scholar
Spark, I.S.C. & Trewin, N.H. (1986) Facies-related diagenesis in the main Claymore Oilfield sandstones. Clay Miner. 21, 479–496.Google Scholar
Środoń, J. J. (1980) Precise identification of illite/smectite interstratification by X-ray powder diffraction. Clays Clay Miner. 28 401-411.Google Scholar
Środoń, J. J. (1984) Mixed-layer illite-smectite in lowtemperature diagenesis: data from the Miocene of the Carpathian foredeep. Clay Miner. 19, 205–215.Google Scholar
Tompkins, R.E. (1981) Scanning electron microscopy of regular chlorite/smectite (corrensite) from a hydrocarbon reservoir sandstone. Clays Clay Miner. 29, 233–235.Google Scholar
Turner, P. (1980) Continental red beds. Developments in Sedimentology, 29, Elsevier Scientific Publishing Company, Amsterdam.Google Scholar
Walker, T.R. (1976) Diagenetic origin of continental red beds. Pp. 240—282 in: The Continental Permian in Central, West, and South Europe (Falke, H., editor). D. Reidel Publishing Company, Dordrecht, The Netherlands.Google Scholar
Waples, D.W. (1985) Geochemistry in Petroleum Exploration. Geological Science Series, International Human Resources Development Corporation, Boston.CrossRefGoogle Scholar
Weibel, R. (1998) Diagenesis in oxidising and locally reducing conditions - an example from the Triassic Skagerrak Formation, Denmark. Sedim. Geol. 121, 259–276.Google Scholar
Wilson, M.D. & Pittman, E.D. (1977) Authigenic clays in sandstones: recognition and influence on reservoir properties and paleoenvironmental analysis. J. Sedim. Petrol. 47, 3–31.Google Scholar