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Diagenetic history of Lower Palaeozoic sediments in Pomerania (northern Poland), traced across the Teisseyre–Tornquist tectonic zone using mixed– layer illite– smectite

Published online by Cambridge University Press:  09 July 2018

J. Środoń  and
N. Clauer
J. Środoń*
Affiliation:
Institute of Geological Sciences PAN, Senacka 1, 31-002 Kraków, Poland
N. Clauer
Affiliation:
Centre de Géochimie de la Surface (CNRS-ULP), EOST, 1 rue Blessig, 67084 Strasbourg, France
*
*E-mail: [email protected]
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Abstract

Mixed-layer illite-smectite from Lower Palaeozoic sedimentary rocks, on both sides of the Teisseyre–Tornquist tectonic zone (TTZ) in northern Poland, was studied by X-ray diffraction and dated by K-Ar means.

The percentage of smectite layers in illite-smectite (%S) indicates maximum palaeotemperatures of 125–135°C at the surface of Lower Palaeozoic rocks on the craton (NE of TTZ), and 110 to ≤180°C in different tectonic blocks to the SW of TTZ (area of Caledonian consolidation). The vertical changes in the %S indicate that the maximum palaeotemperatures were reached before Permian time on the craton, and before Jurassic, Triassic, Permian or Carboniferous periods but after the beginning of Devonian time in the Caledonian zone. The K—Ar ages of bentonites indicate that the maximum palaeotemperatures were reached by 370—390 Ma or even slightly earlier (Middle—late Devonian). A maximum of 3—6 km of Silurian–Devonian cover on the craton and in the TTZ is suggested by the data.

Keywords

diagenesisPalaeozoicPomeraniaPolandTeisseyre–Tornquist zoneillite-smectite
Type
Research Article
Information
Clay Minerals , Volume 36 , Issue 1 , March 2001 , pp. 15 - 27
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2001

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References

Bethke, C.M & Marshak, S. (1990) Brine migrations across North America the plate tectonics of groundwater. Ann. Rev. Earth Planet. Sci. 18, 287–315.Google Scholar
Bonhomme, M., Thuizat, R., Pinault, Y., Clauer, N., Wendling, R. & Winkler, R. (1975) Méthode de datation potassium-argon. Appareillage et technique. Note technique Inst. Géol., Univ. Strasbourg, 3.Google Scholar
Chaudhuri, S.,Środoń, J. & Clauer, N. (1999) K-Ar dating of illitic fractions of Estonian ‘Blue Clay’ treated with alkylammonium cations. Clays Clay Miner. 47, 96–102.CrossRefGoogle Scholar
Clauer, N., Środoń, J., Francu, J. & Šucha, V. (1997) K-Ar dating of illite fundamental particles separated from illite-smectite. Clay Miner. 32, 181–196.CrossRefGoogle Scholar
Clauer, N., Rinckenbach, T., Weber, F., Sommer, F., Chaudhuri, S. and O’Neil, J.R. (1999) Diagenetic evolution of clay minerals in oil-bearing Neogene sandstones and associated shales from Mahakam Delta Basin (Kalimantan, Indonesia). Am. Assoc. Petrol. Geol. Bull. 83, 62–87.Google Scholar
Dadlez, R. (1978) Sub-Permian rock formations in Koszalin- Chojnice zone. Geol. Quarterly, 22, 267–298.(in Polish).Google Scholar
Duane, M.J. & de Wit, M.J. (1988) Pb-Zn ore deposits of the northern Caledonides: Products of continentalscale fluid mixing and tectonic expulsion during continental collision. Geology, 16, 999–1002.Google Scholar
Gee, D.G. & Zeyen, H.J. (1996) EUROPROBE 1996 – Lithosphere Dynamics: Origin and Evolution of Continents. EUROPROBE Secretariate, Uppsala Univ.Google Scholar
Hagenfeldt, S. (1997) Lower Palaeozoic acritarchs as indicators of heat flow and burial depth of sedimentary sequences in Scandinavia. Acta Universitatis Carolinae Geologica, 40, 413–424.Google Scholar
Howard, J.J. (1981) Lithium and potassium saturation of illite/smectite clays from interlaminated shales and sandstones. Clays Clay Miner. 29, 136–142.Google Scholar
Jackson, M.L. (1975) Soil Chemical Analysis – Advanced Course. Published by the author, Madison, WI.Google Scholar
Jensenius, J. (1987) Regional studies of fluid inclusions in Paleozoic sediments from southern Scandinavia. Bull. Geol. Soc. Denmark, 36, 221–235.Google Scholar
Karnkowski, P.H. (1999) Origin and evolution of the Polish Rotliegend Basin. Polish Geol. Inst. Spec. Paper, 3.Google Scholar
Kirsimäe, K., Jørgensen, P. & Kalm, V. (1999) Lowtemperature diagenetic illite-smectite in Lower Cambrian clays in North Estonia. Clay Miner. 34, 151–163.CrossRefGoogle Scholar
Kobyłecka, A. (1994) Diagenesis of flysch sandstones and shales from the borehole Kuz´mina 1. MSc thesis, Jagellonian Univ., Kraków (in Polish).Google Scholar
Lindgreen, H., Drits, V.A., Sakharov, B.A. & Salyn, A.L. (2000) Illite-smectite structural changes during diagenesis of Lower Paleozoic black Alum Shales from the Baltic area. Am. Miner. 85, 1223–1238.Google Scholar
èydka, K., Arakeljanc, M.M. & Milovski, A.V. (1980) The age of anchimetamorphism of the Cambrian and Uppermost Precambrian sediments of the Peribaltic Syneclize (northern Poland). Bull. Acad. Polon. Sci., Ser. Sci. Terre, 28, 1–9.Google Scholar
Modliński, Z. (1976) Some aspects of the structure of the western part of the Peri-Baltic Syneclise. Biul. IG, 270, 37–44.(in Polish).Google Scholar
Mukhopadhyay, P.K. (1994) Vitrinite reflectance as maturity parameter. Pp. 1–24 in. Vitrini te Reflecta nce as a Maturity Parameter (Mukhopadhyay, P.K. and Dow, W.G., editors). ACS Symp. Series, 570. American Chemical Society, Washington, D.C.CrossRefGoogle Scholar
Nehring-Lefeld, M., Modliński, Z. & Swadowska, E. (1997) Thermal evolution of the Ordovician in the western margin of the East-European Platform: CAI and R0 data. Geol. Quarterly, 41, 129–138.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
Środoń, J. (1980) Precise identification of illite/smectite interstratifications by X-ray powder diffraction. Clays Clay Miner. 28, 401–411.Google Scholar
Środoń, J. (1981) X-ray identification of randomly interstratified illite/smectite in mixtures with discrete illite. Clay Miner. 16, 297–304.Google Scholar
Środoń, J. (1984) X-ray powder diffraction identification of illitic materials. Clays Clay Miner. 32, 337–349.Google Scholar
Środoń, J. (1995) Reconstruction of maximum paleotemperatures at present erosional surface of the Upper Silesia Basin, based on the composition of illite/smectite in shales. Studia Geol. Pol. 108, 9–22.Google Scholar
Steiger, R.H. & Jäger, E. (1977) Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planet. Sci. Lett. 36, 359–362.Google Scholar
Šucha, V., Kraus, I., Gerthofferova, H., Petes, J. & Serekova, M. (1993) Smectite to illite conversion in bentonites and shales of the East Slovak Basin. Clay Miner. 28, 243–253.Google Scholar
Suggate, R.P. (1998) Relations between depth of burial, vitrinite reflectance and geothermal gradient. J. Petrol. Geol. 21, 5–32.Google Scholar
Tullborg, E.-L., Larson, S.-A., Bjorklund, L., Samuelsson, L. & Stigh, J. (1995) Thermal evidence of Caledonide foreland, molasse sedimentation in Fennoscandia. SKB Technical Report 95-18. Stockholm: Swedish Nuclear Fuel and Waste Management Co.Google Scholar
Whitney, G. & Northop, H.R. (1987) Diagenesis and fluid flow in the San Juan Basin, New Mexico – regional zonation in the mineralogy and stable isotope composition of clay minerals in sandstone. Am. J. Sci. 287, 253–282.Google Scholar
Znosko, J. (1969) Geology of Kujawy and Eastern Wielkopolska. Pp. 5–48 in: Proc. 41st Conf. Polish Geol. Soc.(Żyłka, R., editor). Wydawnictwa Geologiczne, Warsaw (in Polish).Google Scholar
Zwingmann, H., Clauer, N. & Gaupp, R. (1999) Structurerelated geochemical (REE) and isotopic (K-Ar, Rb- Sr, δ18O) characteristics of clay minerals from Rotliegend sandstone rerservoirs (Permian, northern Germany). Geochim. Cosmochim. Acta, 63, 2805–2823.Google Scholar