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A SEM study of diagenetic kaolinization and illitization of detrital feldspars in sandstones

Published online by Cambridge University Press:  09 July 2018

S. Morad
Affiliation:
Department of Mineralogy and Petrology, Institute of Geology, Uppsala University, Box 555, S-751, 22 Uppsala, Sweden
A. A. AlDahan
Affiliation:
Department of Mineralogy and Petrology, Institute of Geology, Uppsala University, Box 555, S-751, 22 Uppsala, Sweden

Abstract

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Type
Notes
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

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References

AlDahan, A.A. & Morad, S. (1986) Mineralogy and chemistry of diagnetic clay minerals in Proterozoic sandstones from Sweden. Am. J. Sci. 286, 2980.Google Scholar
Chou, L. & Wollast, R. (1985) Steady-state kinetics and dissolution mechanisms of albite. Am. J. Sci. 285, 963993.CrossRefGoogle Scholar
De Vore, G.W. (1959) The surface chemistry of feldspars as an influence on their decomposition products. Clays Clay Miner. 6, 2641.Google Scholar
Güven, N., Hower, W.F. & Davies, D.K. (1980) Nature of authigenic illite in sandstone reservoirs. J. Sedim. Petrol 50, 761766.Google Scholar
Haszeldine, R.S., Samson, I.M. & Cornford, C. (1984) Quartz diagenesis and convective fluid movement: Beatrice Oilfield, UK North Sea. Clay Miner. 19, 391402.Google Scholar
McHardy, W.J., Wilson, M.J. & Tait, J.M. (1982) Electron microscope and X-ray diffraction studies of filamentous illitic clay from sandstones of the Magnus Field. Clay Miner. 17, 2339.Google Scholar
Morris, R.C., Proctor, K.E. & Koch, M.R. (1979) Petrology and diagenesis of deep-water sandstones, Ouachita Mountains, Arkansas and Oklahoma. Pp. 263279 in: Aspects of Diagenesis (Scholle, P. A. and Schluger, P. R., editors). SEPM Spec. Publ. 26.Google Scholar
Morad, S. (1983) Diagenesis and geochemistry of the Visingö Group (Upper Proterozoic), southern Sweden: A clue to the origin of color differentiation. J. Sedim. Petrol. 53, 5165.Google Scholar
Nadeau, P.H. (1985) The physical dimensions of fundamental clay particles. Clay Miner. 20, 499514.Google Scholar
Odom, I.E., Willand, T.N. & Lassin, R.J. (1979) Paragenesis of diagenetic minerals in the St. Peter Sandstone (Ordovician), Wisconsin and Illinois. Pp. 425443 in: Aspects of Diagenesis(Scholle, P. A. and Schluger, P. R., editors). SEPM Spec. Publ. 26.Google Scholar
Tillman, R.W. & Almon, W.R. (1979) Diagenesis of Frontier Formation offshore bar sandstones, Spearhead Ranch Field, Wyoming. Pp. 337378 in: Aspects of Diagenesis. SEPM Spec. Publ. 26.CrossRefGoogle Scholar
Tazaki, K. (1968) Observation of primitive clay precursors during microcline weathering. Cont. Miner. Petrol. 92, 8688.Google Scholar
Velbel, M.A. (1983) A dissolution-reprecipitation mechanism for the pseudomorphous replacement of plagioclase feldspar by clay minerals during weathering. Sci. Géol. Mem. 1, 139147.Google Scholar
Walker, T.R., Waugh, B. & Grone, A.J. (1978) Diagensis in first-cycle desert alluvium of Cenozoic age, southwestern United States and northwestern Mexico. Geol. Soc. Am. Bull. 89, 1932.Google Scholar