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The Polish Sudetes: Caledonian or Variscan?

Published online by Cambridge University Press:  03 November 2011

P. Aleksandrowski ,
R. Kryza ,
S. Mazur ,
C. Pin  and
J. A. Zalasiewicz
J. A. Zalasiewicz
Affiliation:
Uniwersytet Wroclawski, Instytut Nauk Geologicznych, Cybulskiego 30, 50-205 Wroclaw, Poland Département de Géologie, UMR 6524 CNRS, Université Blaise Pascal, 5 rue Kessler, 63 038 Clermont-Ferrand Cedex, France Orogenic Processes Group, Department of Geology, University of Leicester, University Road, Leicester, LEI 7RH, U.K.
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Abstract

The Polish Sudetes on the NE margin of the Bohemian Massif comprise a complex mosaic of pre-Permian basement units, traditionally included in the Variscides. A hypothesis of significant Caledonian orogenesis in this area originated in the 1920s, was subsequently rejected, and then was recently revived in models which invoked Early Palaeozoic to Early-Mid Devonian subduction and continental collision along a proposed extension of the Tornquist suture zone. We reassess the evidence invoked in support of the Caledonian orogeny, such as supposed regional pre-Upper Devonian unconformity, Ordovician bimodal magmatism and radiometric, palaeontological, palaeomagnetic and structural data, and suggest these are either inconclusive or misinterpreted. On the other hand, the Sudetes record Mid?-Late Devonian blueschist metamorphism followed by an Early Carboniferous regional high temperature event, widespread Late Devonian/Early Carboniferous flysch/molasse sedimentation and abundant granite intrusion in the Carboniferous to Early Permian. We discuss the usage of the term ‘Caledonian’ in a plate tectonic context and suggest it should not be used simply to denote Early to Mid-Palaeozoic tectonic activity. The tectonic evolution of the Sudetes was temporally different from, and resulted from convergence of different crustal domains than that of the British-Scandinavian-Pomeranian Caledonides. The Sudetic Palaeozoic sequences most probably developed on Armorican Neoproterozoic crust and in adjacent oceanic(?) domains and, therefore, the Sudetes form part of the Variscan orogenic belt.

Keywords

ArmoricaBohemian MassifEast AvaloniametamorphismPalaeozoicSW Polandradiometric/isotopic datatectonicsterranesTornquist SutureRheic Ocean.
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 90 , Issue 2 , 1999 , pp. 127 - 146
Copyright
Copyright © Royal Society of Edinburgh 1999

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References

Aleksandrowski, P. 1990. Early Carboniferous strike-slip displacements at the northeast periphery of the Variscan Belt in Central Europe. In International Conference on Paleozoic Orogens in Central Europe (IGCP Program 233: Terranes in the Circum-Atlantic Paleozoic Orogens), Abstracts, 7–10. Göttingen: Giessen.Google Scholar
Aleksandrowski, P. 1994. Discussion on U-Pb ages from SW Poland: evidence for a Caledonian suture zone between Baltica and Gondwana. Journal of the Geological Society, London 151, 1049–50.Google Scholar
Aleksandrowski, P. 1995. Rola wielkoskalowych przemieszczeń przesuwczych w uksztaltowaniu waryscyjskiej struktury Sudetów [The significance of major strike-slip displacements in the development of Variscan structure of the Sudetes, SW Poland]. Przegiąd Geologiczny 43, 745–54.Google Scholar
Aleksandrowski, P. 1998. Pre-Variscan and Variscan terranes in SW Poland. In Linnemann, U.et al. (eds) Abstracts of the International Geological Conference Pre-Variscan Terrane Analysis of ‘Gondwanan Europe’, Dresden, Germany. Schriften des Staatlichen Museums für Mineralogie und Geologie zu Dresden 90, 93–5.Google Scholar
Aleksandrowski, P., Kryza, R., Mazur, S.Żaba, J. 1997. Kinematic data on major Variscan strike-slip faults and shear zones in the Polish Sudetes, northeast Bohemian Massif. Geological Magazine 134, 727-39.Google Scholar
Aleksandrowski, P.Żaba, J. 1995. Przełom Bobru poniżej zapory w Pilchowicach. Przekrój przez uskok śródsudecki [Gorge of the Bóbr River below Pilchowice Dam. Transect across the Intra-Sudetic Fault]. In Mierzejewski, M. P. (ed.) Wybrane zjawiska tektoniczne w masywach granitoidowych Dolnego Sląska [Tectonic Structures in Granitoid Massifs of Lower Silesia, SW Poland], Field Guide to Geological Conference, University of Wrocław, 71–4.Google Scholar
Altenberger, U.Besch, T. 1993. The Böllstein Odenwald: evidence for pre- to Early Variscan plate convergence in the Central European Variscides. Geologische Rundschau 82, 475–88.CrossRefGoogle Scholar
Anderle, H. J., Franke, W.Schwab, M. 1995. III.C. Metamorphic Units (N Phyllite Zone). 1. Stratigraphy. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 99–107. Berlin: Springer.CrossRefGoogle Scholar
Awdankiewicz, M. 1997. Petrology and geochemistry of the Carboniferous and Permian rocks of northern part of the Intrasudetic Basin, SW Poland (Unpublished Ph.D. Thesis, University of Wrocław, Poland).Google Scholar
Bachtadse, V., Schätz, M. R., Zwing, A., Tait, J. A., Soffel, H. C. 1998. Paleogeography of the Paleozoic Terranes in the Variscan and Alpine Foldbelts. In Franke, W., Herzberg, S. (eds) SPP ‘Orogene Processe’ 7. Kolloquium, Giessen. Terra Nostra 98/2, 12–15.Google Scholar
Bankwitz, P., Bankwitz, E., Kramer, W. Pin, C. 1994. Early Palaeozoic bimodal volcanism in the Vesser area, Thuringian Forest, eastern Germany. Zentralblatt für Geologie und Paläontologie 1992 I, 1113–32.Google Scholar
Baranowski, Z., Haydukiewicz, A., Kryza, R., Lorenc, S., Muszyński, A., Solecki, A.Urbanek, Z. 1990. Outline of the geology of the Góry Kaczawskie (Sudetes, Poland). Neues Jahrbuch für Geologie und Palaeontologie, Abhandlungen 179, 223–57.Google Scholar
Bederke, E. 1924. Das Devon in Schlesien und das Alter der Sudetenfaltung. Fortschritte der Geologie und Paläontologie H. 7, 1–50.Google Scholar
Bederke, E. 1929. Die varistische Tectonik der mittleren Sudeten. Fortschritte der Geologie und Paläontologie 23, 429–524.Google Scholar
Belka, Z., Ahrend, H., Franke, W., Schäfer, J., Wemmer, K. 1998. Accretion of first Gondwana-derived terranes at the margin of Baltica. In Franke, W., Herzberg, S. (eds) SPP ‘Orogene Processe’ 7. Kolloquium, Giessen. Terra Nostra 98/2, 24–7.Google Scholar
Belka, Z.Siewniak-Madej, A. 1996. Thermal maturation of the Lower Palaeozoic strata in the southwestern margin of the Małopolska Massif, southern Poland: no evidence for Caledonian regional metamorphism. Geologische Rundschau 85, 775–81.CrossRefGoogle Scholar
Berdan, J. M. 1990. The Silurian and Early Devonian biogeography of ostracodes in North America. In McKerrow, W. S., Scotese, C. R. (eds) Palaeozoic Palaeogeography and Biogeography. Geological Society, London, Memoir 12, 105–21.Google Scholar
Bernard-Griffiths, J., Cantagrel, J. M.Duthou, J. L. 1977. Radiometric evidence for an Acadian tectonometamorphic event in western French Massif Central. Contributions to Mineralogy & Petrology 61, 199–212.CrossRefGoogle Scholar
Bernhard, F., Klötzli, U. S., Thöni, M.Hoinkes, G. 1996. Age, origin and geodynamic significance of a polymetamorphic felsic intrusion in the ötztal Crystalline Basement, Tirol, Austria. Mineralogy and Petrology 58, 171–96.CrossRefGoogle Scholar
Bertrand, M. 1887. La chaîne des Alpes et la formation du continent Européen. Bulletin de la Société Géologique de France, Série 3 12, 318–30.Google Scholar
Bogacz, W.Krokowski, J. 1981. Rotation of the basement of the Upper Silesian Coal Basin. Annales Societatis Geologorum Poloniae 51, 361–81.Google Scholar
Borkowska, M., Hameurt, J.Vidal, Ph. 1980. Origin and age of Izera gneisses and Rumburk granites in the Western Sudetes. Ada Geologica Polonica 30, 121–46.Google Scholar
Borkowska, M., Choukroune, P., Hameurt, J.Martineau, F. 1990. A geochemical investigation of the age, significance and structural evolution of the Caledonian-Variscan granite-gneisses of the Śnieżnik metamorphic area, Central Sudetes. Geologia Sudetica 25, 1–27.Google Scholar
Brochwicz-Lewiński, W., Pożaryski, W.Tomczyk, H. 1981. Wielkoskalowe ruchy przesuwcze wzdłuż SW brzegu platformy wschodnioeuropejskiej we wczesnym paleozoiku [Large-scale strike-slip displacements along the SW border of the East European Platform in Early Palaeozoic times]. Przegiąd Geologiczny 29, 385–96.Google Scholar
Brochwicz-Lewiński, W., Tomczyk, H 1983. Ruchy przesuwcze w poludniowej Polsce w paleozoiku [Strike-slip motions in southern Poland in Palaeozoic times]. Przegiąd Geologiczny 31, 651–8.Google Scholar
Bröcker, M., Żelaźniewicz, A.Enders, M. 1998. Rb-Sr and U-Pb geochronology of migmatitic layers from the Góry Sowie (West Sudetes, Poland): the importance of Mid-Late Devonian meta-morphism. Journal of the Geological Society, London 155, 1025–36.CrossRefGoogle Scholar
Brueckner, H. K.Bakun-Czubarow, N. 1991. Zoned Sm/Nd and 143Nd/144Nd ratios in garnets from peridotites of the Caledonides of Norway and the Variscides of Poland. Terra Abstracts, Supplement 6 to Terra Nova 3.Google Scholar
Brueckner, H. K., Medaris, L. G., Bakun-Czubarow, N. 1991. Nd and Sr age and isotope patterns from Variscan eclogites of the eastern Bohemian Massif. Neues Jahrbuch für Mineralogie, Abhandlungen 163, 169–96.Google Scholar
Brueckner, H. K., Blusztajn, J.Bakun-Czubarow, N. 1996. Trace element and Sm-Nd ‘age’ zoning in garnets from peridotites of the Caledonian and Variscan mountains and tectonic implications. Journal of Metamorphic Geology 14, 61–73.CrossRefGoogle Scholar
Buch L., von 1802. Entwurf einer geognostischer Beschreibung von Schlesien. In Buch L., vonGeognostische Beobachtungen auf Reisen durch Deutschland und Italien. 1er Band, 1–132. Berlin: Haude und Spener.Google Scholar
Bukowy, S. 1964. Nowe poglądy na budowę północno-wschodniego obrzeżenia Górnośląskiego Zagłębia Węglowego [New ideas concerning the structure of the NE margin of the Upper Silesia Coal Basin]. Biuletyn Instytutu Geologicznego 184, 5–20.Google Scholar
Bukowy, S. 1984. Struktury waryscyjskie regionu śląsko-krakowskiego [Variscan structures of the Upper Silesia-Cracow region]. Prace Uniwersytetu Śląskiego 69, 1–75.Google Scholar
Buła, Z. 1994. Problemy stratygrafii i wykształcenia osadów starszego paleozoiku północno-wschodniego obrżezenia Górnośląskiego Zagłębia Węglowego [Problems of stratigraphy and development of Lower Palaeozoic sediments of the NE margin of the Upper Silesian Coal Basin]. In Rózkowski, A., Ślósarz, J.Żaba, J. (eds) Paleozoik pólnocno-wschodniego obrzeżenia Górnośląskiego Zaglębia Węglowego. Field Guide, Polish Geological Society 65th Annual Meeting. Prace Uniwersytetu Śląskiego 1431, 31–57. Katowice: Uniwersytet Śląski.Google Scholar
Buła, Z.Jachowicz, M. 1996. The Lower Palaeozoic sediments in the Upper Silesian Block. Geological Quarterly 40, 299–335.Google Scholar
Buła, Z., Jachowicz, M.Żaba, J. 1997. Principal characteristics of the Upper Silesian Block and Małopolska Block border zone (southern Poland). Geological Magazine 134, 669–77.CrossRefGoogle Scholar
Bussy, F., Deron, M. H., Jacquod, J., Sartori, M.Tellin, P. 1996. The 500 Ma-old Thyon metagranite: a new A-type granite occurrence in the western Penninic Alps (Wallis, Switzerland). European Journal of Mineralogy 8, 565–75.CrossRefGoogle Scholar
Chaloupsky, J. 1966. Kaledonska a variska orogeneze v Ještedskem krystaliniku [Caledonian and Variscan orogenies in the Ješted crystalline complex]. Sbornik Geologickych Věd, Seria Geologie 10, 7–38.Google Scholar
Chaloupsky, J. 1988. Caledonian folding in the Bohemian Massif. In Harris, A. L., Fettes, D. J. (eds) The Caledonian-Appalachian Orogen. Geological Society Special Publication 38, 493–8.CrossRefGoogle Scholar
Chaloupsky, J. 1989. Geological evolution of the Krkonoše-Jizerské hory crystalline complex in the Precambriam and Early Paleozoic. In Chaloupsky, J. (ed.) Geologie Krkonoš a Jizerskych hor, 247–77. Praha: Akademia.Google Scholar
Chlupač, I. 1993. Stratigraphic evaluation of some metamorphic units in the N part of the Bohemian Massif.). Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 188, 363–88.Google Scholar
ChlupaČ, I.Hladil, J. 1992. New Devonian occurrences in the Ješted Mts, North Bohemia. Časopis pro Mineralogii a Geologii 37, 185–91.Google Scholar
Cocks, L. R. M.Fortey, R. A. 1982. Faunal evidencefor oceanic separation in the Palaeozoic of Britain. Journal of the GeologicalSociety, London 139, 465–78.CrossRefGoogle Scholar
Corfu, F. Grunsky, E. C. 1987. Igneous and tectonicevolution of the Batchawana greenstone belt, Superior Province: a U-Pb zircon and titanite study. Journal of Geology 95, 87–105.CrossRefGoogle Scholar
Corfu, F.Muir, T. L. 1989. The Helmo-Heron Bay greenstone belt and Hemlo Au-Mo deposit, Superior Province, Ontario, Canada. 1. Sequence of igneous activity determined by zircon U-Pb geochronology. Chemical Geology (Isotope Geoscience Section) 79, 183–200.Google Scholar
Cymerman, Z. 1993. Czy w Sudetach istnieje nasunięcie ramzowskie?[Does the Ramzova Overthrust in the Sudetes actually exist?]. Przegląd Geologiczny 41, 700–6.Google Scholar
Cymerman, Z.Piasecki, M. A. J. 1994. The terrane concept in the Sudetes, Bohemian Massif. Geological Quarterly 38, 191–210.Google Scholar
Cymerman, Z., Piasecki, M. A. J.Seston, R. 1997. Terranes and terrane boundaries in the Sudetes, northeast Bohemian Massif. Geological Magazine 134, 717–25.CrossRefGoogle Scholar
Dadlez, R., Kowalczewski, Z.Znosko, J. 1994. Some key problems of the pre-Permian tectonics of Poland. Geological Quarterly 38, 169–90.Google Scholar
Dallmeyer, R. D.Tucker, R. D. 1993. U-Pb zircon age for the Lagoa augen gneiss, Morais complex, Portugal: tectonic implications. Journal of the Geological Society, London 150, 405–10.CrossRefGoogle Scholar
Dombrowski, A., Henjes-Kunst, F., Höhndorf, A., Kröner, A., Okrusch, M.Richter, P. 1995. Orthogneisses in the Spessart Crystalline Complex, north-west Bavaria: Silurian granitoid magmatism at anactive continental margin. Geologische Rundschau 84, 399–411.CrossRefGoogle Scholar
Don, J. 1984. Kaledonidy i waryscydy Sudetó;w Zachodnich [The Caledonides and Variscides in the Western Sudetes]. Przegląd Geologiczny 8–9, 459–68.Google Scholar
Don, J. 1990. The differences in Paleozoic facies-structural evolution of the West Sudetes. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 307–28.Google Scholar
Don, J.Lorenc, S. 1995. Gibt es einen ostvariscischen Bogen? Nova Acta Leopoldina N.F. 71, 73–85.Google Scholar
Don, J., Dumicz, M., Wojciechowska, I.Żelaźniewicz, A. 1990. Lithology and tectonics of the Orlica-Śnieżnik Dome, Sudetes: recent state of knowledge. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 159–88.Google Scholar
Dörr, W., Pique, A., Franke, W.Kramm, U. 1992. Les galets granitiques du congloméat de Russ (Dévono-Dinantien des Vosgesdu Nord) sont les témoins d’un magmatisme acide ordovicien. La distension crustale et le rifting saxothuringien au Paléozoique inférieur. Comptes Rendus de l’Academie des Sciences de Paris 315 II, 587–94.Google Scholar
Dudek, A. 1980. The crystalline basement block of the Outer Carpathians in Moravia: Bruno-Vistulicum. Rozpravy Česke akademie Věd 90, 1–85.Google Scholar
Dvořak, J. 1995. VIII. Moravo-Silesian Zone. B. Autochthon. 1. Stratigraphy. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 411–89. Berlin: Springer.Google Scholar
Dvořak, J.Paproth, E. 1988. Trends of the Variscan development near the East European Platform. Zeitschrift für Angewandte Geologie 34, 353–9.Google Scholar
Dziedzic, K.Teisseyre, A. K. 1990. The Hercynian molasse and younger deposits in the Intra-Sudetic Depression, SW Poland. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 285–305.Google Scholar
Faure, M., Leloix, Ch.Roig, J-Y. 1997. L’évolution polycyclique de la chaîne hercynienne. Bulletin de la Societé Géologique de France 168, 695–705.Google Scholar
Franke, D. 1995. IX The North Variscan Foreland. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 554–66. Berlin: Springer.CrossRefGoogle Scholar
Franke, W. 1989. Tectonostratigraphic units in the Variscan belt of central Europe. Geological Society of America Special Paper 230, 67–90.CrossRefGoogle Scholar
Franke, W. 1998. Exhumation of HP rocks in the Saxothuringian belt: sedimentary and tectonic record. In Franke, W., Herzberg, S. (eds) SPP ‘Orogene Processe’ 7. Kolloquium, Giessen. Terra Nostra 98/2, 46–8.Google Scholar
Franke, W., Żelaźiewicz, A., Porębski, S. J.Wajsprych, B. 1993. Saxothuringian zone in Germany and Poland: differences and common features. Geologische Rundschau 82, 583–99.CrossRefGoogle Scholar
Franke, W., Dallmeyer, R. D.Weber, K. 1995a. XI. Geodynamic evolution. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 579–93. Berlin: Springer.CrossRefGoogle Scholar
Franke, W., Kreuzer, H., Okrusch, M., Schüssler, U.Seidel, E. 1995b. V. Saxothuringian Basin. C. Exotic metamorphic nappes. 1. Stratigraphy, structure and igneous activity. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 277–94. Berlin: Springer.CrossRefGoogle Scholar
Furnes, H., Kryza, R., Muszyński, A., Pin, C.Garmann, L. B. 1994. Geochemical evidence for progressive, rift-related early Paleozoic volcanism in the western Sudetes. Journal of the Geological Society, London 151, 91–109.CrossRefGoogle Scholar
Galle, A.Chlupač, I. 1976. Finds of corals in the metamorphic Devonian of the Ještědské pohořri Mountains. Věstnik Ústřledniho Ústavu Geologickeho 51, 123–7.Google Scholar
Giese, U., Katzung, G., Walter, R.Weber, J. 1997. The Caledonian deformation of the Brabant Massif and the Early Palaeozoic in northeast Germany: compared. Geological Magazine 134, 637–52.CrossRefGoogle Scholar
Grygar, R.Vavro, M. 1995. Evolution of Lugosilesian orocline (north-eastern periphery of the Bohemian Massif): kinematics of Variscan deformation. Journal of the Czech Geological Society 40, 65–90.Google Scholar
Guillot, F., Liégeois, J. P.Fabre, J. 1991. Des granophyres du Cambrien terminal dans le Mont Pourri (Vanoise, zone briançonnaise): premiere datation U-Pb sur zircon d’un socle des zones internes des Alpes françaises. Comptes Rendus de I’Academie des Sciences de Paris 313 II, 239–44.Google Scholar
Gunia, T. 1985. Pozycja geologiczna bloku sowiogórskiego i jego wplyw na paleogeografię paleozoiku Sudetów Środkowych [Geological position of the Sowie Góry block and its influence on the palaeography of the Palaeozoic complexes of Central Sudetes]. Geologia Sudetica 20, 83–119.Google Scholar
Gunia, T.Wojciechowska, I. 1971. Zagadnienie wieku wapieni i fyllitów z Małego Bożkowa, Sudety Srodkowe [On the age of limestones and phyllites from Maty Bożków, Central Sudetes]. Geologia Sudetica 5, 137–64.Google Scholar
Gürich, G. 1902. Zur Discussion üer das Profil von Ebersdorf. Zeitschrift der Deutschen Geolgischen Gesellschaft 54, 57–63.Google Scholar
Harańczyk, C. 1979. Metallogenic evolution of the Silesia-Cracow region. Prace Instytutu Geologicznego 95, 109–32.Google Scholar
Harańczyk, C. 1982. Krakowidy jako górotwór kaledoński [Cracovides as a Caledonian orogenic belt]. Przegląd Geologiczny 30, 575–81.Google Scholar
Haydukiewicz, A. 1987. Melanże Gór Kaczawskich [Melanges of the Göry Kaczawskie Mts]. In Baranowski, Z. (ed.) Przewodnik LVIII Zjazdu Polskiego Towarzystwa Geologicznego [Field Guide of the Polish Geological Society 58th Meeting]. Kraków, 106–14.Google Scholar
Haydukiewicz, J. 1990. Stratigraphy of Paleozoic rocks of the Góry Bardzkie and some remarks on their sedimentation. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 275–84.Google Scholar
Haydukiewicz, A.Urbanek, Z. 1986. Zmetamorfizowaneskały dewońskie we wschodniej części jednostki Bolkowa, Góry Kaczawskie [The metamorphosed Devonian rocks in the Bolków Unit, the Kaczawskie Mountains, Sudetes]. Geoiogia Sudetica 20, 185–96.Google Scholar
Heinisch, H.Schmidt, K. 1976. Zur kaledonischen Orogenese in den Ostalpen. Geologische Rundschau 65, 459–82.CrossRefGoogle Scholar
Hladil, J., Mazur, S., Galle, A.Ebert, J. 1999. Revised age of the Maly Bożków limestone in the Kodzko metamorphic unit (Early Givetian, late Middle Devonian): implications for the geology of the Sudetes. Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 211, 329–53.CrossRefGoogle Scholar
Howell, D. G. 1995. Principles of Terrane Analysis. New Applications for Global Tectonics, 2nd edn. London: Chapman & Hall.Google Scholar
Jarmolowicz-Szulc, K. 1984. Geochronologiczne studium części północnej osłony granitu Karkonoszy za pomocą metod trakowych [Geochronological study of a part of the northern cover of the Karkonosze Granite by fission track methods]. Archiwum Mineralogiczne 39, 139–83.Google Scholar
Johnston, J. D., Tait, J. A., Oliver, G. J. H.Murphy, J. C. 1994. Evidence for a Caledonian orogeny in Poland. Transactions of the Royal Society of Edinburgh: Earth Sciences 85, 131–42.CrossRefGoogle Scholar
Johnston, J. D., Tait, J. A., Oliver, G. J. H.Murphy, J. C. 1996. Reply to Comments by M. Moczydłowska. Transactions of the Royal Society of Edinburgh: Earth Sciences 86, 231–2.CrossRefGoogle Scholar
Jowett, E. C.Jarvis, G. T. 1984. Formation of foreland rifts. Sedimentary Geology 40, 51–72.CrossRefGoogle Scholar
Jurkiewicz, H. 1975. Budowa geologiczna podłoza mezożoiku centralnej części niecki miechowskiej [Geology of the Mesozoic substratum in the central part of the Miechów depression]. Biuletyn Instytutu Geologicznego 283, 5–96.Google Scholar
Katzung, G., Giese, U., Walter, R.Von Winterfeld, C. 1993. The Rügen Caledonides, northeast Germany. Geological Magazine 130, 725–30.CrossRefGoogle Scholar
Kober, L. 1921. Der Bau der Erde. Berlin: Borntraeger.Google Scholar
Kodym, O.Svoboda, J. 1948. Kaledonska přikrovova stavba Krkonoš a Jizerskych hor. Sbornik Statniho Geologickeho Ustavu CSR 15, 109–80.Google Scholar
Kossmat, F. 1927. Gliederung des varistischen Gebirgsbaues. Abhandlungen Sächsischen Geologischen Landesamts 1, 1–39.Google Scholar
Kowalczewski, Z. 1990. Grubookruchowe skały kambru na środkowym południu Polski. Prace Państwowego Instytutu Geologicznego 131, 1–82.Google Scholar
Krejci-Graf, K. 1950. über die Phasen der Gebirgsbildung. Geologische Rundschau 38, 112–24.CrossRefGoogle Scholar
Kröner, A.Hegner, E. 1998. Geochemistry, single zircon ages and Sm—Nd systematics of granitoid rocks from the Góry Sowie (Owl Mts), Polish West Sudetes: evidence for early Palaeozoic arc-related plutonism. Journal of the Geological Society, London 155, 711–24.CrossRefGoogle Scholar
Kröner, A., Hegner, E., Hammer, J., Haase, G., Bielicki, K.-H., Krauss, M.Eidam, J. 1994a. Geochronology and Nd-Sr systematics of Lusatian granitoids: significance for the evolution of the Variscan orogen in east-central Europe. Geologische Rundschau 83, 357–76.CrossRefGoogle Scholar
Kröner, A., Hegner, E.Jaeckel, P. 1994b. Pb—Pb and U—Pb zircon ages and Nd isotopic systematics for metamorphic rocks from the Góry Sowie Block, West Sudetes, Poland, and geodynamic significance. Journal of the Czech Geological Society, Abstract Volume 39/1, 60.Google Scholar
Kröner, A., Hegner, E., Opletal, M., Schulmann, K.Štipska, P. 1999. Which geodynamic scenario produced the Early Palaeozoic granitoids in the Bohemian Massif? In Old Crust—New Problems, 89th Annual Meeting of the Geologische Vereinigung e.V., Abstracts and Programme (International Colloquium ‘Orogenic Processes: Quantification and modelling in the Variscan Belt’), Freiberg. Terra Nostra 99/1, 129.Google Scholar
Krs, M., Hladil, J., Krsova, M.Pruner, P. 1995. Paleomagnetický doklad pro variskou paleotektonickou rotaci moravských devonských hornin [Palaeomagnetic evidence for Variscan palaeotectonic rotation of Moravian Devonian rocks]. Geologický Výzkum na Moravé a Slezsku 1994, 53–7.Google Scholar
Kryza, R. 1981. Migmatytyzacja w gnejsach północnej części Gór Sowich. [Migmatization in gneisses of the northern part of the Sowie Góry, Sudetes]. Geoiogia Sudetica 14, 7–100.Google Scholar
Kryza, R. 1993. Zasadowe skay metawulkaniczne środkowej części Gór Kaczawskich: studium petrologiczne. Basic metavolcanic rocks of the central Kaczawa Mts (Sudetes): a petrological study]. Prace Geologiczno-Mineralogiczne 39, Wydawnictwo U.Wr., 1–139.Google Scholar
Kryza, R.Mazur, S. 1995a. Przełom Bobru pomiędzy Ciechanowicami a Janowicami Wielkimi. Kontakt wschodniej okrywy granitu Karkonoszy z metamorfikiem Gór Kaczawskich w strefie uskoku śródsudeckiego [Górge of the Bóbr River between Ciechanowice and Janowice Wielkie. Contact of the eastern envelope of the Karkonosze Granite with the Kaczawa Metamorphic Complex across the Intra-Sudetic Fault]. In Mierzejewski, M. P. (ed.) Wybrane zjawiska tektoniczne w masywach granitoidowych Dolnego Śląska [Tectonic Structures in Granitoid Massifs of Lower Silesia, SW Poland], Field Guide to Geological Conference, University of Wrocław, 59–70.Google Scholar
Kryza, R.Mazur, S. 1995b. Contrasting metamorphic paths in the SE part of the Karkonosze-Izera block (Western Sudetes, SW Poland). Neues Jahrbuch für Mineralogie, Abhandlungen 169, 157–92.Google Scholar
Kryza, R.Muszyńiski, A. 1992. Pre-Variscan volcanic-sedimentary succession of the central southern Góry Kaczawskie, SW Poland: outline geology. Annales Societatis Geologorum Poloniae 62, 117–40.Google Scholar
Kryza, R.Pin, C. 1997. Cambrian/Ordovician magmatism in the Polish Sudetes: no evidence for subduction-related setting. In Abstract Supplement 1, EUG9, Strasbourg. Terra Nova 90, 144.Google Scholar
Kryza, R., Muszyńiski, A.Vielzeuf, D. 1990. Glaucophane-bearing assemblage overprinted by greenschist-facies metamorphism in the Variscan Kaczawa complex, Sudetes, Poland. Journal of Metamorphic Geology 8, 345–355.CrossRefGoogle Scholar
Kryza, R., Muszyńiski, A., Turniak, K.Zalasiewicz, J. A. 1994. A Lower Palaeozoic shallow-water sequence in the eastern European Variscides (SW Poland): provenance and depositional history. Geologische Rundschau 83, 5–19.CrossRefGoogle Scholar
Kryza, R., Mazur, S.Pin, C. 1995. Leszczyniec meta-igneous complex in the eastern part of the Karkonosze Izera Block, Western Sudetes: trace element and Nd isotope study. Neues Jahrbuch für Mineralogie, Abhandlungen 170, 59–74.CrossRefGoogle Scholar
Kryza, R., Awdankiewicz, H., Awdankiewicz, M., Kozdrój, W., Szczepański, J.Turniak, K. 1996a. Geotectonic significance of Palaeozoic volcanism in the West Sudetes. In Abstracts, Europrobe Transeuropean Suture Zone Workshop, Książ, 11–17 April 1996. Wrocław.Google Scholar
Kryza, R., Pin, C.Vielzeuf, D. 1996b. High pressure granulites from the Sudetes (SW Poland): evidence of crustal subduction and collisional thickening in the Variscan Belt. Journal of Metamorphic Geology 14, 531–46.CrossRefGoogle Scholar
Kumpera, O. 1983. Geologie spodniho karbonu jesenickeho bloku. Praha: Knihovna Ustředniho Ustavu Geologickeho 59.Google Scholar
Kutek, J.Głazek, J. 1972. The Holy Cross area, Central Poland, in the Alpine cycle. Acta Geologica Polonica 22, 603–53.Google Scholar
Lewandowski, M. 1994. Palaeomagnetic constraints for Variscan mobilism of the Upper Silesian and Małopolska Massifs, southern Poland. Geological Quarterly 38, 211–30.Google Scholar
Liew, T. C.Hofmann, A. W. 1988. Precambrian crustal components, plutonic associations, plate environment of the Hercynian Fold Belt of central Europe: Indications from a Nd and Sr study. Contributions to Mineralogy and Petrology 98, 129–38.CrossRefGoogle Scholar
Linnemann, U.Buschmann, B. 1995. Die cadomische Diskordanz im Saxothuringikum (oberkambrisch-tremadocische overlap-Sequenzen). Zeitschrift für Geologischen Wissenschaften 23, 707–27.Google Scholar
Linnemann, U., Gehmlich, M., Tichomirova, M., Buschmann, B. 1998. The Peri-Gondwanan basement of the Saxothuringian Composite Terrane. In Linnemann, U., et al. (eds) Pre-Variscan Terrane Analysis of ‘Gondwanan Europe’, International Geological Conference, Excursion Guides Abstracts. Schriften des Staatlichen Museums für Mineralogie und Geologie zu Dresden 90, 7–13.Google Scholar
Maluski, H.Patočka, F. 1997. Geochemistry and 40Ar- 39Ar geochronology of the mafic metavolcanic rocks from the Rýchory Mountains complex (West Sudetes, Bohemian Massif): palaeotectonic significance. Geological Magazine 134, 703–16.CrossRefGoogle Scholar
Maluski, H., Rajlich, P.Souček, J. 1995. Pre-Variscan, Variscan and early Alpine thermo-tectonic history of the north-eastern Bohemian Massif: An 40Ar/39Ar study. Geologische Rundschau 84, 345–58.CrossRefGoogle Scholar
Matte, Ph. 1986. Tectonics and plate tectonic model for the Variscan Belt of Europe. Tectonophysics 177, 329–74.CrossRefGoogle Scholar
Matte, Ph. 1991. Accretionary history and crustal evolution of the Variscan Belt in Western Europe. Tectonophysics 196, 309–37.CrossRefGoogle Scholar
Matte, Ph., Maluski, H., Rajlich, P.Franke, W. 1990. Terrane boundaries in the Bohemian Massif: results of large-scale Variscan shearing. Tectonophysics 177, 151–70.CrossRefGoogle Scholar
Mazur, S. 1995. Strukturalna i metamorficzna ewolucja wschodniej okrywy granitu Karkonoszy w południowej części Rudaw Janowickich i Grzbiecie Lasockim. [Structural and metamorphic evolution of the country rocks at the eastern contact of the Karkonosze granite in the southern Rudawy Janowickie Mts and Lasocki Range]. Geoiogia Sudetica 29, 31–98.Google Scholar
Mazur, S.Kryza, R. 1996. Superimposed compressional and extensional tectonics in the Karkonosze-Izera Block, NE Bohemian Massif. In Oncken, O.Janssen, C. (eds) Basement Tectonics 11, Europe and Other Regions. Proc. 11th Int. Conf. on Basement Tectonics, Potsdam, 51–66. Dordrecht: Kluwer.CrossRefGoogle Scholar
Mazur, S.Puziewicz, J. 1995. Mylonity strefy Niemczy [Mylonites of the Niemcza Fault Zone]. Annales Societatis Geologorum Poloniae 64, 23–52.Google Scholar
Mazur, S., Aleksandrowski, P.Awdankiewicz, M. 1998. The South and East Karkonosze metamorphic complexes (Western Sudetes): a Variscan suture zone modified by extensional collapse. Acta Universitatis Carolinae—Geologica 42(2), 304–5.Google Scholar
McKerrow, W. S.Ziegler, A. M. 1972. Palaeozoic oceans. Nature 240, 92–4.Google Scholar
Mierzejewski, M. P.Oberc-Dziedzic, T. 1990. The Izera-Karkonosze Block and its tectonic development (Sudetes, Poland). Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 197–222.Google Scholar
Misař, Z. 1995. VIII. Moravo-Silesian Zone. C. Allochthonous Units. 1. Stratigraphy. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 521–9. Berlin: Springer.CrossRefGoogle Scholar
Mizerski, W. 1979. Tectonics of the Lysogóry unit in the Holy Cross Mts. Acta Geologica Polonica 29, 1–38.Google Scholar
Mizerski, W. 1988. Ewolucja tektoniczna regionu łysogórskiego Gór Świętokrzyskich [Tectonic evolution of the Łysogóry region, Holy Cross Mts]. Przegtąd Geologiczny 36, 46–52.Google Scholar
Mizerski, W. 1994. Ewolucja paleotektoniczna kambru świętokrzyskiego [Palaeotectonic evolution of the Holy Cross Cambrian]. Przegląd Geologiczny 42, 721–7.Google Scholar
Moczydłowska, M. 1993. Is there Caledonian deformation in the TESZ (Trans-European Suture Zone of Upper Silesia, southern Poland?) In Gee, D. G., Beckholmen, M. (eds), Europrobe Symposium, Jablonna 1991. Publications of the Institute of Geophysics, Polish Academy of Sciences a–20 (255), 199–22.Google Scholar
Moczydłowska, M. 1995. Neoproterozoic and Cambrian successions deposited on the East European Platform and Cadomian basement area in Poland. Studia Geophysica et Geodetica 39, 276–85.CrossRefGoogle Scholar
Moczydłowska, M. 1996. Comments on ‘Evidence for a Caledonian orogeny in Poland’ by Johnston, J. D., Tait, J. A., Oliver, J. H. and, Murphy, F. G.. Transactions of the Royal Society of Edinburgh: Earth Sciences 86, 227–30.CrossRefGoogle Scholar
Moczydłowska, M. 1997. Proterozoic and Cambrian successions in Upper Silesia: an Avalonian terrane in southern Poland. Geological Magazine 134, 679–89.CrossRefGoogle Scholar
Muszyńiski, A. 1994. Kwaśne skaly metawulkanogeniczne środkowej części Gór Kaczanskich: Studium petrologiczne [Acid metavolcanogenic rocks of the central Kaczawa Mts, Sudetes: a petrological study]. Seria Geologia 15. Poznań: Wydawnictwo Naukowe Uniwersytetu Adama Mickiewicza.Google Scholar
Narębski, W. 1980. Paleotectonic setting of circum-Karkonosze spilitekeratophyre suites based on the geochemistry of iron group elements. Annales Societatis Geologorum Poloniae 50, 3–25.Google Scholar
Narębski, W. 1994. Lower to Upper Paleozoic tectonomagmatic evolution of NE part of the Bohemian Massif. Zentralblatt für Geologie und Paläontologie 1992 1, 961–72.Google Scholar
Narębski, W., Dostal, J.Dupuy, C. 1986. Geochemical characteristis of Lower Paleozoic spilite-keratophyre series in the Western Sudetes (Poland): petrogenetic and tectonic implications. Neues Jahrbuch für Mineralogie, Abhandlungen 155, 243–58.Google Scholar
Narębski, W., Wojciechowska, I.Dostal, J. 1989. Initial rifting volcanics in the Kłodzko Metamorphic Complex (Polish Middle Sudetes), evidenced by geochemical data. Bulletin of the Polish Academy of Sciences, Earth Sciences 36, 261–9.Google Scholar
Nowak, J. 1927. Zarys tektoniki Polski [Esquisse de la téctonique de la Pologne], Kraków: II Zjazd Slowiańskich Geografów i Etnografów.Google Scholar
Oberc, J. 1966. Geologia krystaliniku WzGórz Strzelińskich [Geology of the crystalline rocks of the Wzgórza Strzelińskie Hills, Lower Silesia]. Studia Geologica Polonica 20, 1–187.Google Scholar
Oberc, J. 1968. Granica między strukturą zachodnio- i wschodniosudecką [The boundary between the Western and Eastern Sudetic tectonic structures]. Annales Societatis Geologorum Poloniae 38, 203–17.Google Scholar
Oberc, J. 1972. Budowa Geologiczna Polski, IV. Tectonika, 2. Sudety i obszary przylegle. Warszawa: Wydawnictwa Geologiczne.Google Scholar
Oberc, J. 1977. Besteht ein kaledonisches Tektogen in Südpolen. Neues Jahrbuch für Geologie und Paläontologie, Monatshefte 1, 56–63.Google Scholar
Oberc, J. 1980. Early to Middle Variscan development of the West Sudetes. Acta Geologica Polonica 30, 27–52.Google Scholar
O'Brien, P. J.Carswell, D. A. 1993. Tectonometamorphic evolution of the Bohemian Massif: evidence from high pressure metamorphic rocks. Geologische Rundschau 82, 531–55.CrossRefGoogle Scholar
O'Brien, P. J., Kröner, A., Jaeckel, P., Hegner, E., Źelaźniewicz, A.Kryza, R. 1997. Petrological and isotopic studies on Palaeozoic high-pressure granulites, Góry Sowie Mts, Polish Sudetes. Journal of Petrology 38, 433–456.CrossRefGoogle Scholar
Oliver, G. J. H.Kelley, S. 1993. 40Ar39Ar fusion ages from the Polish Sudetes: Variscan tectonothermal reworking of Caledonian protoliths. Neues Jahrbuch für Geologie und Paläontologie, Monatshefte 1993, 321–44.CrossRefGoogle 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. Journal of the Geological Society, London 150, 355–69.CrossRefGoogle Scholar
Oliver, G. J. H., Corfu, F.Krogh, T. E. 1994. Discussion on U-Pb ages from SW Poland: evidence for a Caledonian suture zone between Baltica and Gondwana. Journal of the Geological Society, London 151, 1052–3.Google Scholar
Pagel, M., Costa, S., Galibert, F., Lancelot, J., Maluski, H., Meyer, A.Turpin, L. 1992. Forage scientifique de Sancerre-Couy: Géochronologie Sm-Nd, U-Pb, Ar-Ar, Rb-Sr et chronométrie par traces de fission sur le socle. Géologie de la France 3/4, 129–34.Google Scholar
Parry, M., Štipska, P., Schulmann, K., Hrouda, F., Ježek, JKröner, A. 1997. Tonalite sill emplacement at an oblique plate boundary: northeastern margin of the Bohemian Massif. Tectonophysics 280, 61–81.CrossRefGoogle Scholar
Patočka, F.Valenta, J. 1996. Geochemistry of the late Devonian intermediate to acid metavolcanic rocks from the southern part of the Vrbno Group, the Jeseniky Mts. (Moravo-Silesian Belt, Bohemian Massif, Czech Republic): paleotectonic implications. Geolines 4, 42–54.Google Scholar
Pearce, J. A., Harris, N. B. W.Tindle, A. G. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology 25, 956–83.CrossRefGoogle Scholar
Pin, C. 1990. Variscan oceans: Ages, origins and geodynamic implications inferred from geochemical and radiometric data. Tectonophysics 177, 215–27.CrossRefGoogle Scholar
Pin, C.Marini, F. 1993. Early Ordovician continental break-up in Variscan Europe: Nd-Sr isotope and trace element evidence from bimodal igneous associations of the Southern Massif Central, France. Lithos 29, 177–96.CrossRefGoogle Scholar
Pin, C.Vielzeuf, D. 1983. Granulites and related rocks in Variscan median Europe: a dualistic interpretation. Tectonophysics 93, 47–74.CrossRefGoogle Scholar
Pin, C., Majerowicz, A.Wojciechowska, I. 1988. Upper Palaeozoic oceanic crust in the Polish Sudetes: Nd-Sr isotope and trace element evidence. Lithos 21, 195–209.CrossRefGoogle Scholar
Pin, C., Puziewicz, J.Duthou, J.-L. 1989. Ages and origins of a composite granitic massif in the Variscan belt: a Rb-Sr study of the Strzegom-Sobótka Massif, West Sudetes (Poland). Neues Jahrbuch für Mineralogie, Abhandlungen 160, 71–82.Google Scholar
Pin, C., Ortega-Cuesta, L. A.Gil, Ibarguchi J. I. 1992. Mantlederived, early Palaeozoic A-type metagranitoids from the NW Iberian Massif: Nd-isotope and trace element constraints. Bulletin de la Société Géologique de France 163, 483–94.Google Scholar
Pitcher, W. S. 1993. The nature and origin of granites. Glasgow & London: Blackie.CrossRefGoogle Scholar
Pitcher, W. S., Atherton, E. J., Cobbing, E. J.Beckinsale, R. D. (eds) 1985. Magmatism at a plate edge the Peruvian Andes. Glasgow & London: Blackie.CrossRefGoogle Scholar
Porębski, S. J. 1981. Sedymentacja utworów górnego dewonu i dolnego karbonu depresji Świebodzic, Sudety Zachodnie [Świebodzice succession, Devonian-lowermost Carboniferous, Western Sudetes: a prograding mass-flow dominated fan-delta complex]. Geologia Sudetica 16, 101–92.Google Scholar
Porębski, 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 Świebodzice succession. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 259–74.Google Scholar
Pożaryski, W. 1977. The Caledonian and Variscan Epochs in the Epi-Gothian Platform and its border zone. In Pożaryski, W. (ed.) Geology of Poland, IV Tectonics, 175–252. Warsaw: Wydawnictwa Geologiczne.Google Scholar
Pożaryski, W. 1990. Kaledonidy środkowej Europy—orogenem przesuwczym zlożonym z terranów [Caledonides of the Central Europe as a strike-slip collage]. Przegląd Geologiczny 38, 1–9.Google Scholar
Pożaryski, W. 1997. Tektonika powaryscyjska obszaru świętokrzyskolubelskiego na tle struktury podłoża [Post-Variscan tectonics of the Holy Cross Mts—Lublin region, central Poland, and the basement structure]. Przegląd Geologiczny 45, 1265–70.Google Scholar
Pożaryski, W.Karnkowski, P. 1992. Tectonic map of Poland during the Variscan epoch, 1:1,000,000. Warszawa: Wydawnictwa Geologiczne.Google Scholar
Přichystal, A. 1990. Hlavni vysledky studia paleozoickeho vulkanismu ve šternbersko-hornobenešovskem pruhu, Nizky Jesenik [Principal results of a study of the Paleozoic volcanism in the Šternberk-Horni Benešov belt, the Nizky Jesenik Mts.]. Sbornik Geologickych Věd, Ložiskova Geologie, Mineralogie 29, 41–66.Google Scholar
Přichystal, A. 1996. Geochemistry and geotectonic setting of Paleozoic volcanism in the Moravo-Silesian region. Polskie Towarzystwo Mineralogiczne, Prace Specjalne 8, 94–6.Google Scholar
Reischmann, T.Anthes, G. 1996. Geochronology of the mid-German crystalline rise west of the river Rhine. Geologische Rundschau 85, 761–74.CrossRefGoogle Scholar
Rey, P., Burg, J.-P., Casey, M. 1997. The Scandinavian Caledonides and their relationship to the Variscan belt. In Burg, J.-P., Ford, M. (eds) Orogeny Through Time, 179–200. Geological Society Special Publication 121.Google Scholar
Ryka, W. 1973. Metamorficzne skały kaledońiskiego podłoża w okolicy Zawiercia [Metamorphic rocks of the Caledonian basement in the vicinity of Zawiercie]. Kwartalnik Geologiczny 17, 667–82.Google Scholar
Santos, Zalduegui J. F., Schärer, U.Gil, Ibarguchi J. I. 1995. Isotope constraints on the age and origin of magmatism and metamorphism in the Malpica-Tuy allochthon, Galicia, NW Spain. Chemical Geology 12, 91–103.Google Scholar
Schäfer, J., Neuroth, H., Ahrendt, H.Dörr, W. 1997. Accretion and exhumation at a Variscan active margin, recorded in the Saxothuringian flysch. Geologische Rundschau 86, 599–611.Google Scholar
Scotese, C. R., McKerrow, W. S. 1990. Revised world maps: an introduction. In McKerrow, W. S., Scotese, C. E. (eds) Palaeozoic Palaeogeography and Biogeography. Geological Society, London, Memoir 12, 1–21.Google Scholar
Scotese, C. R., McKerrow, W. S. 1991. Ordovician plate tectonic reconstructions. In Barnes, C. R., Williams, S. H. (eds) Advances in Ordovician Geology. Geological Survey of Canada, Paper 90/9, 271–82.Google Scholar
Şengör, A. M. C. 1990. Plate tectonics and orogenic research after 25 years: a Tehtyan perspective. Earth-Science Reviews 27, 1–201.Google Scholar
Seyler, M. 1986. Petrology and genesis of Hercynian alkaline orthogneisses from Provence, France. Journal of Petrology 27, 1229–51.CrossRefGoogle Scholar
Siebel, W., Raschka, H., Irber, W., Kreuzer, H., Lenz, K.-L., Höhndorf, H.Wendt, I. 1997. Early Palaeozoic acid magmatism in the Saxothuringian Belt: new insights from a geochemical and isotopic study of orthogneisses and metavolcanic rocks from the Fichtelgebirge, SE Germany. Journal of Petrology 38, 203–30.CrossRefGoogle Scholar
Skacel, J. 1989. Hranice Lugika a Silezika (střednich a vychodnich Sudet) [On the Lugicum-Silesicum boundary]. Acta Universitatis Wratislaviensis, Prace Geologiczno-Mineralogiczne 17, 45–55.Google Scholar
Souček, J., Jelinek, E.Bowes, D. R. 1992. Geochemistry of gneisses of the eastern margin of the Bohemian Massif. In Kukal, Z. (ed.) Proceedings of the 1st International Conference on the Bohemian Massif, 269–85, Prague: Czech Geological Survey.Google Scholar
Staszic, S. 1815. O ziemiorodztwie Karpatow i innych gor i rownin Polski. Warszawa: Drukarnia Rządowa.Google Scholar
Steltenpohl, M. G., Cymerman, Z., Krogh, E. J.Kunk, M. J. 1993. Exhumation of eclogitized continental basement during Variscan lithospheric delamination and gravitational collapse, Sudety Mountains, Poland. Geology 21, 1111–14.2.3.CO;2>CrossRefGoogle Scholar
Stille, H. 1924. Grundfragen der Vergleichenden Tektonik. Berlin: Borntraeger.Google Scholar
Stille, H. 1949. Die kaledonische faltung Mitteleuropas im Bilde der gesamteuropäischen. Zeitschrift der Deutschen Geologischen Gesellschaft 100, 223–66.CrossRefGoogle Scholar
Stille, H. 1951. Das mitteleuropäische varistische Grundgebirge im Bilde des gesamteuropäischen. Beiheft zum Geologisches Jahrbuch 2, 1–138.Google Scholar
Stosch, H. G.Lugmair, G. W. 1990. Geochemistry and evolution of MORB-type eclogites from the Münchberg Massif, southern Germany. Earth and Planetary Science Letters 99, 230–49.CrossRefGoogle Scholar
Stupnicka, E. 1992. The significance of the Variscan orogeny in the Świętokrzyskie Mountains (Mid Polish Uplands). Geologische Rundschau 81, 561–70.CrossRefGoogle Scholar
Suess, E. 1888. Das Antlitz der Erde, Vol. II. Wien: Tempsky.Google Scholar
Suess, E. 1901. Das Antlitz der Erde, Vol. III. Wien: Tempsky.Google Scholar
Suess, F. E. 1912. Die moravischen Fenster und ihre Beziehung zum Grundgebirge des Hohes Gesenkes. Denkschrifte der österreichischen Akademie der Wissenschaften 78, 541–631.Google Scholar
Suess, F. E. 1926. Intrusionstektonik und Wandertektonik im variszischen Grundgebirge. Berlin: Borntraeger.CrossRefGoogle Scholar
Suess, F. E. 1935. Der lugische Bau in seinem Verhältnis zur variszischen Orogenese. Mitteilungen der Geologischen Gesellschaft in Wien 28, 1–36.Google Scholar
Tait, J. A. 1986. A new interpretation for the geology of the Pilchowice Zapora area, SW Poland. (Unpublished B.Sc. Honours Thesis, St. Andrews University, Scotland).Google Scholar
Tait, J. A., Bachtadse, V.Soffel, H. 1996. Eastern Variscan fold belt: Paleomagnetic evidence for oroclinal bending. Geology 24, 871 4.2.3.CO;2>CrossRefGoogle Scholar
Tait, J. A., Bachtadse, V., Franke, W.Soffel, H. C. 1997. Geodynamic evolution of the European Variscan fold belt: palaeomagnetic and geological constraints. Geologische Rundschau 86, 585–98.CrossRefGoogle Scholar
Teisseyre, H. 1956. Kaledonidy sudeckie i ich waryscyjska przebudowa [Sudetic Caledonides and their Variscan reworking]. Przegląd Geologiczny 4, 97–104.Google Scholar
Teisseyre, H. 1957. Sudety. A. Część pierwsza. Opis ogólny. In Książkiewicz, M. (ed.) Regionalna Geologia Polski. T. III. Sudety, Z. 1. Utwory przedtrzeciorzędowe, 9–23. Kraków: Państwowe Wydawnictwo Naukowe.Google Scholar
Teisseyre, H. 1960. The principal structural features of the Sudetic Caledonides. In Report of the International Geological Congress, 21st Session, Norden, Pt. 19, Caledonian Orogeny, 108–9. Copenhagen.Google Scholar
Teisseyre, H. 1976. Das Problem der Hauptfaltung in den Sudeten. Nova Acta Leopoldina N.F. 224, 83–92.Google Scholar
Teisseyre, H. 1980. Precambrian in South-Western Poland. Geologia Sudetica 15, 7–42.Google Scholar
Teisseyre, J. 1973. Skały metamorficzne Rudaw Janowickich i Grzbietu Lasockiego [Metamorphic rocks of the Rudawy Janowickie and Lasockie Grzbiet ranges]. Geologia Sudetica 8, 7–120.Google Scholar
Timmermann, H., Parrish, R. R., Noble, S. R.Kryza, R. 1999. Single cycle Variscan orogeny inferred from new U-(Th-)Pb data from the Sudetes Mountains in Poland and the Czech Republic. In EUG 10 Meeting, Terra Abstracts 11, 95.Google Scholar
Todt, W. A., Altenberger, U.Raumer J. F., von 1995. U-Pb data on zircons for the thermal peak of metamorphism in the Variscan Odenwald, Germany. Geologische Rundschau 84, 466–72.Google Scholar
Tomczyk, H. 1988. Region łysogórski a platforma wschodnioeuropejska w cyklu kaledońsko-waryscyjskim [Łysogóry region and East European Platform during the Caledonian-Variscan cycle]. Przegląd Geologiczny 36, 9–17.Google Scholar
Torsvik, T. H.Trench, A. 1991. The Ordovician history of the Iapetus Ocean in Britain: new palaeomagnetic constraints. Journal of the Geological Society, London 148, 423–5.CrossRefGoogle Scholar
Torsvik, T. H., Smethurst, M. A., Van, der Voo R., Trench, A., Abrahamsen, N.Halvorsen, E. J. 1992. Baltica: a synopsis of Vendian-Permian palaeomagnetic data and their palaeotectonic implications. Earth-Science Reviews 33, 133–52.CrossRefGoogle Scholar
Torsvik, T. H., Trench, A., Svensson, I.Walderhaug, H. J. 1993. Palaeogeographic significance of mid Silurian palaeomagnetic results from southern Britain—major revision of the apparent polar wander path for Eastern Avalonia. Geophysical Journal International 113, 651–68.CrossRefGoogle Scholar
Turniak, K., Mazur, S., Wysoczanski, R. 1998. SHRIMP zircon geochronology for gneisses from the Orlica-Śnieżnik Dome (West Sudetes, SW Poland): evidence for an Early Palaeozoic (∼ 500 Ma) plutonism and a Viséan (∼ 340 Ma) HT/LP metamorphic event. Europrobe Tesz and Pace TMR network meetings. Abstracts volume, Prague 4–6.10.1998, 25.Google Scholar
Unrug, R.Dembowski, Z. 1971. Rozwój diastroficznosedymentacyjny basenu morawsko-śląskiego [Diastrophic and sedimentary evolution of the Moravia-Silesia Basin]. Rocznik Polskiego Towarzystwa Geologicznego 41, 119–68.Google Scholar
Urbanek, Z. 1978. The significance of Devonian conodont faunas for the stratigraphy of epi-metamorphic rocks of north-eastern part of the Góry Kaczawskie. Geologia Sudetica 13, 7–30.Google Scholar
Urbanek, Z., Źelaźniewicz, A., Kemnitz, H., Hermsdorf, N.Linnemann, U. 1995. VI. Western Sudetes (Lugicum). B. Stratigraphy. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 315–27. Berlin: Springer.CrossRefGoogle Scholar
van, Breemen O., Bowes, D.R., Aftalion, M.Źelaźniewicz, A. 1988. Devonian tectonothermal activity in the Sowie Góry gneissic block, Sudetes, SW Poland: evidence from Rb-Sr and U-Pb isotopic studies. Annales Societatis Geologorum Poloniae 58, 3–19.Google Scholar
Vielzeuf, D.Pin, C. 1989. Geodynamic implications of granulitic rocks in the Hercynian belt. In Daly, J. S., Cliff, R. A.Yardley, B. W. D. (eds) Evolution of Metamorphic Belts. Geological Society Special Publication 43, 343–8. London: Geological Society.Google Scholar
Wajsprych, B. 1978. Allochtoniczne skały paleozoiczne w osadach wizeńskich Gór Bardzkich, Sudety [Allochthonous Paleozoic rocks in the Visean of the Bardzkie Mts, Sudetes]. Rocznik Polskiego Towarzystwa Geologicznego 58, 99–127.Google Scholar
Wajsprych, B. 1986. Sedimentary record of tectonic activity on a Devonian-Carboniferous continental margin, Sudetes. In Teisseyre, A. K. (ed.) IAS 7th Regional Meeting, Excursion Guidebook, 141–64. Kraków & Wrocław: Ossolineum.Google Scholar
Wierzchołowska-Kicułowa, K. 1984. Budowa geologiczna utworów podpermskich monokliny przedsudeckiej [Geology of the pre-Permian succession of the Fore-Sudetic Monocline]. Geologia Sudetica 19, 121–42.Google Scholar
Wieser, T. 1978. Glaucophane schists and associated rocks of Kopina Mt. (Lasocki range, Sudetes). Mineralogia Polonica 90, 35–56.Google Scholar
Wilson, M. 1989. Igneous petrogenesis: A global tectonic approach. London: Harper Collins Academic.CrossRefGoogle Scholar
Winchester, J. A., Floyd, P. A., Chocyk, M., Horbowy, K.Kozdrój, W. 1995. Geochemistry and tectonic environment of Ordovician meta-igneous rocks in the Rudawy Janowickie Complex, SW Poland. Journal of the Geological Society, London 152, 105–15.CrossRefGoogle Scholar
Winchester, J. A., Floyd, P. A., Franke, W., Źelazniewicz, A., Patočka, F., Kryza, R., Cymerman, Z., Piasecki, M. A. J., Seston, R., Crowley, Q. G., Kachlik, V., Štedra, V.Holland, J. G. 1998. A review of recent geochemical and structural evidence for major Palaeozoic rifting and re-assembly within the Bohemian Massif. Acta Universitatis Carolinae—Geologica 42, 359–60.Google Scholar
Wojciechowska, I. 1966. Budowa geologiczna metamorfiku dorzecza Ścinawki Kłodzkiej [Geology of the metamorphic massif in the basin of cinawka Kłodzka], Geologia Sudetica 2, 261–96.Google Scholar
Wojciechowska, I. 1990. Geology of the Kłodzko metamorphic unit (Sudetes, Poland). Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 189–95.Google Scholar
Źaba, J. 1994. Mezoskopowe struktury kwiatowe w dolnopaleozoicznych utworach NE obrzeżenia GZ—rezultat transpresyjnego ścinania w strefie dyslokacyjnej Kraków-Myszków [Mesoscopic flower structures in Lower Palaeozoic deposits of the NE margin of the Upper Silesia Coal Basin—the result of transpressional shearing on the Kraków-Myszków Fault Zone]. Przegiąd Geologiczny 42, 643–8.Google Scholar
Źaba, J. 1995. Uskoki przesuwcze strefy krawędziowej bloków górnośląskiego i małopolskiego [Strike-slip faults at the edge zone of Upper Silesia and Małopolska blocks, southern Poland]. Przegiąd Geologiczny 43, 838–42.Google Scholar
Źaba, J. 1996. Póżnokarbońska aktywność przesuwcza strefy granicznej bloków górnośląskiego i małopolskiego [Late Carboniferous strike-slip activity at the boundary zone of Upper Silesia and Małopolska Blocks]. Przegląd Geologiczny 44, 173–80.Google Scholar
Źaba, J. 1999. Ewolucja strukturalna utworów dolnopaleozoicznych w strefie granicznej bloku Górnośląskiego i małopolskiego [Structural evolution of Lower Palaeozoic deposits in the boundary zone of the Upper Silesia and Małopolska Blocks]. Prace Państwowego lnstytutu Geologicznego 166, 1–162.Google Scholar
Źelaźniewicz, A. 1987. Tektoniczna i metamorficzna ewolucja Gór Sowich [Tectonic and metamorphic evolution of the Góry Sowie Mts]. Annales Societatis Geologorum Poloniae 57, 203–348.Google Scholar
Źelaźniewicz, A. 1990. Deformation and metamorphism in the Góry Sowie gneiss complex, Sudetes, SW Poland. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 179, 129–57.Google Scholar
Źelaźniewicz, A. 1997. The Sudetes as a Palaeozoic orogen in central Europe. Geological Magazine 134, 691–702.CrossRefGoogle Scholar
Źelaźniewicz, A.Franke, W. 1994. Discussion on U-Pb ages from SW Poland: evidence for a Caledonian suture zone between Baltica and Gondwana. Journal of the Geological Society, London 151, 1050–52.Google Scholar
Źelaźniewicz, A., Kemnitz, H.Hermsdorf, N. 1995. VI. Western Sudetes (Lugicum). C. Structure. In Dallmeyer, R. D., Franke, W.Weber, K. (eds) Pre-Permian Geology of Central and Eastern Europe, 328–40. Berlin: Springer.CrossRefGoogle Scholar
Źelaźniewicz, A., Dörr, W., Dubińska, E. 1998. Lower Devonian oceanic crust from U-Pb zircon evidence and Eo-Variscan event in the Sudetes. In Franke, W., Herzberg, S. (eds) SPP ‘Orogene Processe’ 7. Kolloquium, Giessen. Terra Nostra 98/2, 174–6.Google Scholar
Znosko, J. 1984. Tectonics of the southern part of Middle Poland (beyond the Carpathians). Zeitschrift der Deutschen Geologischen Gesellschaft 135, 585–602.CrossRefGoogle Scholar
Znosko, J. 1988. O niektórych interpretacjach tektonicznych Gór Świętokrzyskich. Przegiqd Geologiczny 36, 597–601.Google Scholar
Znosko, J. 1996. Tectonic style of the Early Palaeozoic sequences in the Holy Cross Mountains. Geological Quarterly 40, 1–22.Google Scholar