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Surface temperature, sequence stratigraphy and deep burial diagenesis

Published online by Cambridge University Press:  09 July 2018

R. H. Worden ,
A. H. Ruffell  and
C. Cornford
R. H. Worden*
Affiliation:
School of Geosciences, The Queen's University, Belfast BT7 1NN, UK
A. H. Ruffell
Affiliation:
School of Geosciences, The Queen's University, Belfast BT7 1NN, UK
C. Cornford
Affiliation:
Integrated Geochemical Interpretation Ltd, Hallsannery, Bideford, Devon EX39 5HE, UK
*
*E-mail: r.worden@liv.ac.uk
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Abstract

Fourth-order relative sea level changes may have a significant impact upon burial diagenesis and reservoir quality through their effect upon surface and subsurface temperature. Relative sea level changes can induce sediment surface temperature changes of <20°C when the sediment surface changes from being close to or beneath the thermocline to being sub-aerially exposed. Such sea level changes typically occur on a timescale of half a million years. Approximately one quarter to one third of the magnitude of these temperature fluctuations will be propagated to 2500 m in the subsurface. Shorter timescale fluctuations of similar magnitude, resulting from glaciation, will not be significant below ~1000 m burial as there is not enough time to effect the change before the next surface temperature cycle occurs. Diagenesis is strongly controlled by temperature through its impact on the driving force and rate of geochemical processes. Burial diagenesis and cementation may thus be episodic on timescales associated with sequence stratigraphic events occurring on the surface, thousands of metres above the zone where diagenesis is occurring.

Keywords

sea levelglaciationtemperaturediagenesistransient effects
Type
Research Article
Information
Clay Minerals , Volume 35 , Issue 1 , March 2000 , pp. 13 - 23
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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Footnotes

†

Present address: Department of Earth Sciences, University of Liverpool, Brownlow Street, Liverpool L69 3BX, UK

References

Allen, P.A. & Allen, J.R. (1990) Basin Analysis, Principles and Applications. Blackwell, Oxford.Google Scholar
Andel, T. van. (1985) New Views on an Old Planet. Cambridge University Press, Cambridge.Google Scholar
Andreasen, D.J. & Ravelo, A.C. (1997) Tropical Pacific ocean thermocline depth reconstructions for the last glacial maximum. Paleoceanography, 12, 12–395.Google Scholar
Calder, I.N. (1974) Arithmetic of ice ages. Nature, 252, 252–216.Google Scholar
Carslaw, H.S. & Jaeger, J.G. (1959) Conduction of Heat in Solids. Clarendon Press, Oxford.Google Scholar
Crerar, D., Hellmann, R. & Dove, P. (1988) Dissolution kinetics of albite and quartz in hydrothermal solutions. Chem. Geol. 70, 70–77.Google Scholar
Eilola, K. (1997) Development of a spring thermocline at temperatures below the maximum density with application to the Baltic Sea. J. Geophys. Res. Oceans, 102 C4, 4–8657.Google Scholar
Eisenlohr, B.N., Tompkins, L.A., Cathles, L.M., Barley, M.E. & Groves, D.I. (1994) Mississippi Valley-type deposits: products of brine expulsion by eustatically induced hydrocarbon generation? An example from northwestern Australia. Geology, 22, 22–315.2.3.CO;2>CrossRefGoogle Scholar
Frakes, L.A. & Francis, J.E. (1988) A guide to Phanerozoic polar climates from high-latitude icerafting in the Cretaceous. Nature, 333, 333–547.Google Scholar
Gibbons, K., Hellem, T., Kjemperud, A., Nio, S.D. & Vebenstad, K. (1993) Sequence-architecture, fades development and carbonate-cemented horizons in the troll Field reservoir, offshore Norway. Pp 1-31 in: Advances in Reservoir Geology (Ashton, M., editor). Geological Society of London, Spec. Publ. 69.Google Scholar
Lamb, H.H. (1977) Climate, Past, Present and Future. Methuen.Google Scholar
Lasaga, A.C. & Kirkpatrick, R.J. (1981) Kinetics of Geochemical Processes. Reviews in Mineralogy, 8, Mineral Society of America, Washington D.C.Google Scholar
Miller, A.J., White, W.B. & Cayan, D.R. (1997) North Pacific thermocline variations on ENSO timescales. J. Phys. Oceanography, 27, 27–2023.Google Scholar
Paillet, J. & Mercier, H. (1997) An inverse model of the eastern North Atlantic general circulation aaand thermocline ventilation. Deep Sea Res. (I) Ocean. Res. Papers, 44, 44–1293.Google Scholar
Plint, A.G. (1988) Global eustacy and the Eocene sequence in the Hampshire Basin, England. Basin Res. 1, 1–11.Google Scholar
Podlaha, O.F., Mutterlose, J. & Veizer, J. (1998) Preservation of δ180 and δ13C in belemnite rostra from the Jurassic/early Cretaceous successions. Am. J. Sci. 298, 298–324.Google Scholar
Sclater, 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, 85–3711.Google Scholar
Taylor, K.G., Gawthorpe, R.L. & Vanwagoner, J.C. (1995) Stratigraphie control on laterally persistent cementation, Bookcliffs, Utah. J. Geol. Soc. 152, 152–225 Google Scholar
Walderhaug, O. (1994) Precipitation rates for quartz cementation in sandstones determined by fluid inclusion microthermometry and temperature history modelling. J. Sed. Res. A64, 64–324.Google Scholar
Worden, R.H. & Morad, S. (2000) Quartz cement in oil field sandstones: a review of the critical problems. Pp. 1-20 in: Quartz Cementation in Sandstones (Worden, R.H. & S. Morad, editors). Spec. Publ. Int. Assoc. Sedimentol. 29. Blackwells, Oxford, UK.Google Scholar
Worden, R.H., Oxtoby, N.H. & Smalley, P.C. (1998) Can oil emplacement stop quartz cementation. Petrol. Geosci. 4, 4–129.CrossRefGoogle Scholar
You, Y.Z. (1997) Seasonal variations of thermocline circulation and ventilation in the Indian Ocean. J. Geophys. Res. Oceans, 102 C5, 5–10391.Google Scholar