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Evidence for a Caledonian orogeny in Poland

Published online by Cambridge University Press:  03 November 2011

J. D. Johnston ,
J. A. Tait ,
G. J. H. Oliver  and
F. C. Murphy
J. D. Johnston
Affiliation:
Department of Geology, Trinity College Dublin, Dublin 2, Ireland
J. A. Tait
Affiliation:
Geology Department, St Andrews University, Scotland, KY169ST. (Now at the Institute für Geophysik, Ludwig-Maximilians-Universität, Theresienstr., 37–41, 80333 München, Germany)
G. J. H. Oliver
Affiliation:
Geology Department, St Andrews University, Scotland, KY169ST
F. C. Murphy
Affiliation:
Department of Geology, Jane Herdman Laboratories, PO Box 47, Liverpool, L69 3BX, UK. (Now with Pasminco Exploration, Level 2, The Atrium, 290 Burwood Road, Hawthorn, Victoria 3122, Australia)
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Abstract

The Lower Palaeozoic tectonic history of central and eastern Europe is poorly understood because of extensive Variscan and/or Alpine reworking. The trace of the Tornquist Sea, the SE arm of the Lower Palaeozoic Iapetus Ocean, extended from NE Britain to Asia Minor. The site of this ocean is constrained by the tectonostratigraphy and faunal provinciality of Lower Palaeozoic inliers in northern Czechoslovakia, and southern Poland. In this paper, the collage of contrasting tectonostratigraphic histories of terranes in the Lower Palaeozoic of Poland is reviewed. Fossil evidence demonstrates that the Holy Cross Mountains and the Krakovian Belt display Lower Ordovician and Lower Devonian angular unconformities. Faunal data suggest that the Tornquist Suture Zone must lie south of the Holy Cross and between Upper Silesia and the Barrandian of the Czech Republic. Between these areas, in the Sudeten Mountains, a continental scale sinistral mylonite zone (along the line of the Intra-Sudetic Fault) was periodically active between the Middle Ordovician and the Upper Triassic. Various dismembered ophiolite, island arc and batholith terranes from alongside the Intra-Sudetic Fault have Ordocivian and Silurian magmatic and metamorphic zircon isotopic and fossil ages. Thus the often stated view that deformation in the Sudetes is Variscan (i.e. post-Middle Devonian) must be called into question. It is proposed instead that the Tornquist Suture is located within the Sudeten mountains, and as in the Holy Cross Mountains, much of the observed deformation is post-Cambrian and pre-Gedinnian in age, i.e. Caledonian.

Keywords

Caledonianfaunal provincesIntra-Sudetic FaultmetamorphismSudeten MountainsterranesTornquist Sea closureU-Pb dates
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 85 , Issue 2 , 1994 , pp. 131 - 142
Copyright
Copyright © Royal Society of Edinburgh 1994

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References

Aftalion, M., Bowes, D. R. & Vrana, S. 1989. Early Carboniferous U-Pb zircon age for garnetiferous perpotassic granulites, Blansky les massif, Czechoslovakia. N JB MIN ABH 160, 145–52.Google Scholar
Baranowski, Z. 1988. Lupki Radzimowickie gor Kacawskich (Sudety Zachnodnie) Charakterystyka litofacjalna metamorfizowanych osadur rowu, oceanicznego. ANNS SOC GEOL POLAND 58, 325–83.Google Scholar
Baronowski, Z., Haydukiewicz, A., Kryza, R., Lorenc, S., Muszynski, A., Solecki, A. & Urbanek, Z. 1990. Outline of the geology of the Gory Kaczawskie (Sudetes, Poland). N JB GEOL PAL ABH 179, 223–57.Google Scholar
Bederke, E. 1924. Das Devon in Schlesien und das Alter der Sudetenfaltung. FORTSCH GEOL PALAONT 7.Google Scholar
Bergstrom, S. M. 1990. Relations between conodont provincialism and changing palaeogeography during the Early Palaeozoic. In McKerrow, W. S. & Scotese, C. R. (Eds.) Palaeozoic palaeogeography and biogeography. GEOL SOC LONDON MEM 12, 105–40.CrossRefGoogle Scholar
Borkowska, M, Hemert, J. & Vidal, P. 1980. Origin and age of Izera gneisses and Rumburk Granites in W. Sudetes. ACTA GEOL POL 30, 121–46.Google Scholar
Borkowska, M., Choukroune, P., Hemert, J. & Martineau, F. 1990. A geochemical investigation of the age, significance, and structural evolution of the Caledonian-Variscan granite gneisses of the Snieznik metamorphic area, central Sudetes, Poland. GEOL SUDETICA 25, 1–27Google Scholar
Carswell, D. A. & Jamtveit, B. 1990. Variscan Sm-Nd ages for the high-pressure metamorphism in the Moldanubian zone of the Bohemian Massif, Lower Austria. N JB MIN AB 162, 145–52.Google Scholar
Carswell, D. A. & O'Brien, P. J. 1993. Variscan Sm-Nd ages for the high-pressure metamorphism in the Moldanubian Zone of the Bohemian Massif in Austria. J PETROL 34, 427–59.CrossRefGoogle Scholar
Chab, J. & Vrana, S. 1979. Crossite-actinolite amphiboles of the Karkonosze-Izera crystalline complex and their geological significance. VESTNIK USTREDNNOVO USTAVU GEOLOGICKEHO 54, 143–50.Google Scholar
Cocks, L. B. M. & Fortey, R. A. 1982. Faunal evidence for oceanic separation in the Palaeozoic of Britain. J GEOL SOC LONDON 139, 465–78.CrossRefGoogle Scholar
Cocks, L. B. M. & Fortey, R. A. 1990. Biogeography of Ordovicain and Silurian faunas. In McKerrow, W. S. & Scotese, (Eds) Palaeozoic palaeogeography and biogeography. GEOL SOC LONDON MEM 12, 97–104.CrossRefGoogle Scholar
Dadlez, R., Kowalczewski, Z. & Znosko, J. 1994. Some key problems of pre-Permian tectonics of Poland. GEOL Q PAN INST GEOL 2, 169–90.Google Scholar
Don, J. 1990. The differences in Paleozoic facies-structural evolution of the West Sudetes. N JB GEOL PALAONT ABH 179, 307–28.Google Scholar
Don, J., Dumicz, M., Wojciechowska, I. & Zelazniewicz, A. 1990. Lithology and tectonics of the Orlica-Snieznik Dome, Sudetes Recent state of knowledge. N JB GEOL PAL ABH 179, 159–88.Google Scholar
Franke, D. 1990. Der präpermische Untergrund der Mitteleuropäischen Senke Fakten und Hypothesen. NDS AKAD GEOWIEE VEROFFTL 4, 19–75.Google Scholar
Furnes, H., Kryza, R., Muszynski, A., Pin, C. & Garmann, L. B. 1994. geochemical evidence for progressive, rift-related early Palaeozoic volcanism in the western Sudetes. J GEOL SOC LONDON 151, 91–109.CrossRefGoogle Scholar
Galle, A. & Chlupac, I. 1976. Finds of corals in the metamorphic Devonian of the Jestedske Pohori Mountains. VESTNIK USTREDNNOVO USTAVU GEOLOGICKEHO 51, 123–7.Google Scholar
Guiraud, M. & Burg, J. P. 1984. Mineralogical and petrological study of blueschist meta tuff from the Zelezny Brod Crystalline Complex, Czechoslovakia. N JB MINERAL ABH 149, 1–2.Google Scholar
Guterch, A., Grad, M, Materzok, R. & Perchuc, E. 1986. Deep structure of the earth's crust in the contact zone of the Palaeozoic and Precambrian platforms in Poland (Tornquist-Teisseyre Zone). TECTONOPHYS 128, 295–306.CrossRefGoogle Scholar
Gunia, T. 1981. Microflora from paragneisses of Sowie Gory Mts., Sudetes. GEOL SUDETICA 16, 7–21.Google Scholar
Gunia, T. 1984. Mikraflora z wapieni krystalicznych okolicy Norwego Waliszowa (Krowlarki-metamorphic Snieznieka)-Sudety. GEOL SUDETICA 18, 56–70.Google Scholar
Gunia, T. & Wojciechowska, I. 1971. On the age of limestones and phyllites from Maly Bozkow (central Sudetes). GEOL SUDETICA 5, 137–64.Google Scholar
Haranczyk, C. 1982. Krakowidy jako gorotwor Kaledonski. PREZ GEOL 11, 575–82.Google Scholar
Haydukiewicz, A. 1977. Lithostratigraphy and structural development of the Kaczawa Complex in the Rzeszowek unit and western part of the Jakuszowa unit (the Gory Kaczawskie). GEOL SUDETICA 12, 1–93.Google Scholar
Haydukiewicz, A. & Urbanek, Z. 1986. The metamorphosed Devonian rocks in the Bolkow unit (the Kaczawskie Mts., Sudetes). GEOL SUDETICA 20, 185–96.Google Scholar
Hoffman, N. 1990. Zur palaodynamischen Entwicklung des Prazechsteins in der Nordostdeutschen Senke. NDS AKAD GEOWISS VEROFFTL 4, 5–18.Google Scholar
Hull, J. 1988. Thickness displacement relationships for deformation zones. J STRUCT GEOL 10, 431–5.CrossRefGoogle Scholar
Kodym, O. & Svoboda, J. 1948. Kaledonska Prikrovda Starba Krkonos a Jizerskay Hor. SBORNIK-STATINIHO GEOLOGICKEHO USTAVU REP. CESTOSTOVENSKE 15, 109–60.Google Scholar
Kowalczewski, Z. & Migaszewski, Z. 1993. Key problems of the tectonics and stratigraphy of the Palaeozoic rocks in the Holy Cross Mountains (Gory Swietokryskie), Poland. In Gee, D. G. (Ed.) Europrobe Symposium, Jablonna. PUB INST GEOPHYS POLISH ACAD SCI A–20, (255) 99–104.Google Scholar
Kröner, A., Hegner, E. & Jaeckel, P. 1994a. Pb-Pb and U-Pb zircon ages and Nd Isotopic systematics for metamorphic rocks from the Gory Sowie Block, West Sudetes, Poland, and Geodynamic significance. J CZECH GEOL SOC 39/1, 60.Google Scholar
Kroner, A., Jaeckel, P. & Opetal, M. 1994b. Pb-Pb and U-Pb zircon ages for orthogneisses from eastern Bohemi: further evidence for a major Cambro-Ordovician magmatic event. J CZECH GEOL SOC 39/1, 61.Google Scholar
Kroner, A., Hegner, E., Hammer, J., Hasse, G., Bielicki, K.H., Krauss, M. & Eidam, J. 1994c. Geochronology and Nd-Sr systematics of Lusatian granitoids—significance for the evolution of the Variscan Orogen in East-Central Europe. GEOL RUNDS 83, 357–76.CrossRefGoogle Scholar
Kryza, R. & Muszynski, A. 1992. Pre-Variscan volcanic-sedimentary succession of the central southern Gory Kaczawski, SW Poland: Outline geology. ANNS SOC GEOL POLONIAEI 62, 117–40.Google Scholar
Kryza, R., Muszynski, A. & Furnes, H. 1989. Early Palaeozoic volcanism in the Kaczawa Mountains. Lithological and geochemical correlations between the western parts of the Swierzawa and Bolkov units. In Narebski, W. & Majerowicz, A. (Eds) Lower and Upper Palaeozoic Metabasites and Ophiolites of the Polish Sudetes. Guidebook of Excursions in Poland 1989. Wroclaw: Polish Academy of Science, University of Wroclaw.Google Scholar
Kryza, R., Muszynski, A. & Vielzeuf, D. 1990. Glaucophane-bearing assemblages overprinted by greenschist facies metamorphism in the Variscan Kaczawa complex, Sudetes, Poland. J MET PETROL 8, 345–55.CrossRefGoogle Scholar
Ksiazkiewicz, M., Samsonowicz, J. & Rtihle, E. 1968. An Outline of the Geology of Poland. Warszawa.Google Scholar
Lister, G. S. & Snoke, A. W. 1984. S-C mylonites. J STRUCT GEOL 6, 617–38.CrossRefGoogle Scholar
McKerrow, W. S. & Scotese, C. R. (Eds) 1990. Palaeozoic palaeogeography and biogeography. GEOL SOC LONDON MEM 12.Google Scholar
Matte, P., Maluski, H., Rajlich, P. & Franke, W. 1990. Terrane boundaries in the bohemian massif: result of large scale variscan shearing. TECTONOPHYS 177, 151–70.CrossRefGoogle Scholar
Mierzejewski, A. 1989. Sectorial shortening of Silesian Orogen, movement of the Gory Sowie block and the position of Lower Silesian ophioitic complex. In Narebski, W. & Majerowicz, A. (Eds) Lower and Upper Palaeozoic Metabasites and Ophiolites of the Polish Sudetes. Guidebook of Excursions in Poland 1989. Wroclaw: Polish Academy of Science, University20 of Wroclaw.Google Scholar
Moczydlowska, M. 1993. Is there Caledonian deformation on the TESZ (Trans-European Suture Zone) of Upper Silesia, Southern Poland? In Gee, D. G. (Ed.) Europrobe Symposium, Jablonna. PUB INST GEOPHYS POLISH ACAD SCI A–20 (255), 119–22.Google Scholar
Muszynski, A. & Kryza, R. 1992. First findings of jadeite in the Kaczawa Mts, Sudetes. PRZ GEOL 1, 24–6.Google Scholar
Narebski, W., Dostal, J. & Dupuy, C. 1986. Geochemical characteristics of Lower palaeozoic spilites-keratophyre series in the Western Sudetes (Poland): petrogenetic and tectonic implications. N JB MINERAL ABH 155, 243–58.Google Scholar
Oberc, J. 1977. Besteht ein kaledonisches Tektogen in Siidpolen? N JB PALAONT ABH 1, 56–63.Google Scholar
Oliver, G. J. H., Corfu, F. & Krogh, T. E. 1993. U-Pb ages from SW Poland: evidence for a Caledonian suture zone between Baltica and Gondwana. J GEOL SOC LONDON 150, 355–69.CrossRefGoogle Scholar
Oliver, G. J. H. & Kelley, S. 1993. 40Ar39Ar fusion ages from the Polish Sudetes: Variscan tectonothermal reworking of Caledonian protoliths. N JB GEOL PAL 1993, 321–44.Google Scholar
Orlowski, S. 1975. Lower Cambrian trilobites from Upper Silesia (Goczalkowiece borehole). ACTA GEOLOGIA POLONICA 25, 377–86.Google Scholar
Pin, C, Mierzejewski, M., Dutton, J. L. & Couturie, J. P. 1988. Etude isotopique RbSr du granite de Karkonosze. In Lorenc, S. & Marwerowicz, A. (Eds) Petrologie et Geologie du Scale Varisque de Sudetes Polonaises resuhats de la cooperation entre les Universites de Wroclaw et Clermont-Ferrand, 8–44, Wroclaw.Google Scholar
Porebski, E. 1982. Latest Silurian and early Devonian graptolites from Zdanow section, Bardo Mts. (Sudetes). ANNS SOC GEOL POLONIAE 52, 89–209.Google Scholar
Porebski, S. J. 1990. Onset of coarse clastic sedimentation in the Variscan realm of the Sudetes (SW Poland): an example from the upper Devonian-lower Carboniferous Swiebodzice succession. N JB GEOL PAL 179, 259–74.Google Scholar
Pozaryski, W. 1977. Geology of Poland, Volume 4, Tectonics. Warszawa: WYD GEOL. 718pp.Google Scholar
Rajlich, P. 1990. Variscan shearing kinematics and terranes in the Bohemian Massif. International conference on Paleozoic Orogens in Central Europe, Gottingen-Giessen, Aug/Sept. 1990.Google Scholar
Sawicki, L. 1967. Geological Map of Lower Silesia, 1:200000, Warszawa: WYD GEOL.Google Scholar
Sokolowski, S. 1970. Geology of Poland, Volume 1, Stratigraphy. Warszawa: WYD GEOL.Google Scholar
Soper, N. J., Strachan, R. A., Holdsworth, R. E., Gayer, R. A. & Greiling, R. O. 1992. Sinistral transpression and the Silurian closure of Iapetus. J GEOL SOC LONDON 149, 871–80.CrossRefGoogle Scholar
Suk, M. 1984. Geological History of the Territory of the Czech Socialist Republic. Ustrednovo Ustavu Geologickeho Praha, 396 pp.Google Scholar
Suk, M. & Weiss, J. 1981. Geological sections through the Variscan Orogen in the Bohemian Massif. GEOL MI JNB 60, 161–8.Google Scholar
Tait, J. A. 1986. A new interpretation for the geology of the Pilochowice—Zapora area, south-west Poland. (Unpublished B. Sc. Thesis, University of St Andrews, Scotland).Google Scholar
Teisseyre, H. 1980. Precambrian in South West Poland. GEOL SUDETICA XV, 1–33.Google Scholar
Tuckey, M. E. 1990. Biogeography of Ordovician bryozoans. PALAEOGEOG PALAEOCLIM & PALAEOECOL 77, 91–136.CrossRefGoogle Scholar
Urbanek, Z., Baronowski, Z. & Haydukiewicz, A. 1975. Geological consequences of the occurrence of the Devonian conodonts in metamorphic rocks of the northern part of the Kaczawa Mountains. GEOL SUDET1CA 10, 155–69.Google Scholar
Van Breemen, O., Aftalion, M., Bowes, D. R., Dudek, A., Misra, Z., , Povondra & Vrana, S. 1982. Geochronological studies of the Bohemian massif, Czechoslovakia, and their significance in the evolution of Central Europe. TRANS R SOC EDINBURGH: EARTH SCI 73, 89–108.CrossRefGoogle Scholar
Van Breemen, O., Bowes, D. R., Aftalion, M. & Zelazniewicz, A. 1988. Devonian tectonothermal activity in the Sowie Gora Gneissic Block, Sudetes, SW Poland: evidence from Rb-Sr and U-Pb isotopic studies. ANNS SOC GEOL POLONIAE 58, 3–19.Google Scholar
Wajsprych, B. 1978. Allochtonous Palaeozoic rocks in the Visean of the Gory Bardzkie Mountains, Sudetes. ANN SOC GEOL POLONIAE 58, 99–127.Google Scholar
Wendt, J. I., Kroner, A., Fiala, J. & Todt, W. 1994. U-Pb zircon and Sm-Nd dating of Moldanubian HP/HT granulites from Bohemia. Czech Republic. J GEOL SOC LONDON 151, 83–90.CrossRefGoogle Scholar
Wiesser, T. 1978. Glaucophane schists and associated rocks of Kopina Mt. (Lasocki range, Sudetes). MIN POLONIAE 9, 35–6.Google Scholar
Wojciechowska, I. 1990. Geology of the Klodzko metamorphic unit (Sudetes, Poland). N JB GEOL PAL ABH 179, 189–95.Google Scholar
Zelazniewicz, A. 1987. Tektoniczna i metamorficzna ewolucja gor sowich. ANNS SOC GEOL POLONIAE 57, 203–348.Google Scholar
Znosko, J. 1981. The problem of oceanic crust and of ophiolites in the Sudetes. In Narebski, W. (Ed.) Ophiolites and Initialities of the Northern Border of the Bohemian Massif. Guide Book of Excursions. Acad Sci GDR & Polish Acad Sci Vol II, 3–27.Google Scholar