Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-25T04:52:19.907Z Has data issue: false hasContentIssue false

Multiple Archaean to Early Palaeozoic events of the northern Gondwana margin witnessed by detrital zircons from the Radzimowice Slates, Kaczawa Complex (Central European Variscides)

Published online by Cambridge University Press:  15 October 2007

RAFAŁ TYSZKA
Affiliation:
University of Wrocław, Institute of Geological Sciences, Department of Mineralogy and Petrology, ul. Cybulskiego 30, 50-205 Wrocław, Poland
RYSZARD KRYZA*
Affiliation:
University of Wrocław, Institute of Geological Sciences, Department of Mineralogy and Petrology, ul. Cybulskiego 30, 50-205 Wrocław, Poland
JAN A. ZALASIEWICZ
Affiliation:
University of Leicester, Department of Geology, University Road, Leicester LE1 7RH, UK
ALEXANDER N. LARIONOV
Affiliation:
Centre of Isotopic Research, A.P. Karpinsky All Russian Geological Research Institute (VSEGEI), 74 Sredny Pr, St Petersburg, 199 106, Russia
*
§Author for correspondence: [email protected]

Abstract

SIMS dating of detrital zircons from the stratigraphically enigmatic Radzimowice Slates of the Kaczawa Mountains (Sudetes, SW Poland), near the eastern termination of the European Variscides, has yielded age populations of: (1) 493–512 Ma, corresponding to late Cambrian to early Ordovician magmatism and constraining a maximum depositional age; (2) between 550 and 650 Ma, reflecting input from diverse Cadomian sources; and (3) older inherited components ranging to c. 3.3 Ga, with age spectra similar to those from Gondwanan North Africa. The new data show that the Radzimowice Slates cannot form a Proterozoic base to the Kaczawa Mountains succession, as suggested by earlier models, but was deposited, at the earliest, as an extensional basin-fill, during a relatively late stage of the break-up of this part of northern Gondwana.

Type
Original Article
Copyright
Copyright © Cambridge University Press 2007

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Aleksandrowski, P., Kryza, R., Mazur, S., Pin, C., Zalasiewicz, J. A. 2000. The Polish Sudetes: Caledonian or Variscan? Transactions of the Royal Society of Edinburgh, Earth Sciences 90, 127–46.CrossRefGoogle Scholar
Aleksandrowski, P. & Mazur, S. 2002. Collage tectonics in the northeasternmost part of the Variscan Belt: the Sudetes, Bohemian Massif. In Palaeozoic Amalgamation of Central Europe (eds Winchester, J. A., Pharaoh, T. C. & Verniers, J.), pp. 237–77. Geological Society of London, Special Publication no. 201.Google Scholar
Baranowski, Z. 1988. Lithofacies characteristics of trench-fill metasediments in the Radzimowice Slate (Palaeozoic), Sudetes, SW Poland. Annales Societas Geologorum Poloniae 58, 325–83.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 Mineralogie, Abhandlungen 179, 223–57.Google Scholar
Collins, A. S., Kryza, R. & Zalasiewicz, J. A. 2000. Macrofabric fingerprints of Late Devonian–Early Carboniferous subduction in the Polish Variscides, the Kaczawa complex, Sudetes. Journal of the Geological Society, London 157, 283–8.CrossRefGoogle Scholar
Crowley, Q. G., Floyd, P. A., Winchester, J. A., Franke, W. & Holland, J. G. 2001. Early Palaeozoic rift-related magmatism in Variscan Europe: fragmentation of the Armorican Terrane Assemblage. Terra Nova 12, 171–80.CrossRefGoogle Scholar
Franke, W. & Żelaźniewicz, A. 2000. The eastern termination of the Variscides: terrane correlation and kinematic evolution. In Orogenic Processes: Quantification and Modelling in the Variscan Belt (eds Franke, W., Haak, V., Oncken, O. & Tanner, D.), pp. 6386. Geological Society of London, Special Publication no. 179.Google Scholar
Friedl, G., Finger, F., Paquette, J. L., Von Quadt, A., McNaughton, N. J. & Fletcher, I. R. 2004. Pre-Variscan geological events in the Austrian part of the Bohemian Massif deduced from U–Pb zircon ages. International Journal of Earth Sciences (Geologische Rundschau) 93, 802–23.CrossRefGoogle Scholar
Furnes, H., Kryza, R., Muszyński, A., Pin, C. & Garmann, L. B. 1994. Geochemical evidence for progressive rift-related volcanism in the eastern Variscides. Journal of the Geological Society, London 151, 91109.CrossRefGoogle Scholar
Gradstein, F. M., Ogg, J. G. & Smith, A. G. (eds) 2005. A geologic time scale 2004. Cambridge University Press, 610 pp.CrossRefGoogle Scholar
Inglis, J. D., Samson, S. D., D'lemos, R. S. & Miller, B. V. 2005. Timing of Cadomian deformation and magmatism within La Hague, NW France. Journal of the Geological Society, London 162, 389400.CrossRefGoogle Scholar
Kryza, R., Mazur, S., Aleksandrowski, P., Zalasiewicz, J. A., Sergeev, S. & Presnyakov, S. 2007 a. Early Palaeozoic initial-rift volcanism in the Central European Variscides (the Kaczawa Mountains, Sudetes, SW Poland): evidence from SIMS dating of zircons. Journal of the Geological Society, London 164, in press.CrossRefGoogle Scholar
Kryza, R., Mazur, S. & Oberc-Dziedzic, T. 2004. The Su-detic geological mosaic: insights into the root of the Vari-scan orogen. Przegląd Geologiczny 52 (8/2), 761–73.Google Scholar
Kryza, R. & Muszyński, A. 1992. Pre-Variscan volcanic-sedimentary succession of the central southern Góry Kaczawskie, SW Poland: Outline Geology. Annales Societas Geologorum Poloniae 62, 117–40.Google Scholar
Kryza, R. & Muszyński, A. 2003. Kompleks metamorficzny Gór Kaczawskich – fragment waryscyjskiej pryzmy akrecyjnej. [The metamorphic Kaczawa Complex – fragment of Variscan accretionary prism.] In Sudety Zachodnie: od wendu do czwartorzędu (eds Ciężkowski, W., Wojewoda, J. & Żelaźniewicz, A..), pp. 95104. Wrocław: WIND (in Polish, English summary).Google Scholar
Kryza, R., Zalasiewicz, J. A., Mazur, S., Aleksandrowski, P., Sergeev, S. & Larionov, A. 2007 b. Precambrian crustal contribution to the Variscan accretionary prism of the Kaczawa Mountains (Sudetes, SW Poland): evidence from SHRIMP dating of detrital zircons. International Journal of Earth Sciences (in press, DOI 10.1007/s00531-006-0147-x).CrossRefGoogle Scholar
Larionov, A. N., Andreichev, V. A. & Gee, D. G. 2004. The Vendian alkaline igneous suite of northern Timan: ion microprobe U–Pb zircon ages of gabbros and syenite. In The Neoproterozoic Timanide Orogen of Eastern Baltica (Gee, D. G. & Pease, V. L.), pp. 6974. Geological Society of London, Memoir no. 30.Google Scholar
Linnemann, U., Gehmlich, M., Tichomirova, M., Buschmann, B., Nasdala, L., Jonas, P., Lützner, H. & Bombach, K. 2000. From Cadomian subduction to Early Palaeozoic rifting: the evolution of Saxo-Thuringia at the margin of Gondwana in the light of single zircon geochronology and basin development (Central European Variscides, Germany). In Orogenic Processes: Quantification and Modelling in the Variscan belt (eds Franke, W., Haak, V., Oncken, O. & Tanner, D..), pp. 131–53. Geological Society of London, Special Publication no. 179.Google Scholar
Linnemann, U., McNaughton, N. J., Romer, R. L., Gehmlich, M., Drost, K. & Tonk, C. 2004. West African provenance for Saxo-Thuringia (Bohemian Massif): Did Armorica ever leave pre-Pangean Gondwana? – U/Pb-SHRIMP zircon evidence and the Nd-isotopic record. International Journal of Earth Sciences 93, 683705.CrossRefGoogle Scholar
Ludwig, K. R. 2005 a. SQUID 1.12 A User's Manual. A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication. 22 pp. http://www.bgc.org/klprogrammenu.html.Google Scholar
Ludwig, K. R. 2005 b. User's Manual for ISOPLOT/Ex 3.22. A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication. 71 pp. http://www.bgc.org/klprogrammenu.html.Google Scholar
Mazur, S., Aleksandrowski, P., Kryza, R. & Oberc-Dziedzic, T. 2006. The Variscan Orogen in Poland. Geological Quarterly 50 (1), 89118.Google Scholar
Muszyński, A., Machowiak, K., Kryza, R. & Armstrong, R. 2002. SHRIMP U–Pb geochronology of the late-Variscan Żeleźniak rhyolitic intrusion. W Sudetes – preliminary results. Mineralogical Society of Poland Special Papers 20, 156–8.Google Scholar
Nance, R. D., Murphy, J. B. & Keppie, J. D. 2002. A Cordilleran model for the evolution of Avalonia. Tectonophysics 352, 1131.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
Pereira, M. F., Chichorro, M., Linnemann, U., Eguiluz, L. & Silva, J. B. 2006. Inherited arc signature in Ediacaran and Early Cambrian basins of the Ossa-Morena Zone (Iberian Massif, Portugal): Paleogeographic link with European and North African Cadomian correlatives. Precambrian Research 144, 297315.CrossRefGoogle Scholar
Samson, S. D., D'Lemos, R. S., Miller, B. V. & Hamilton, M. A. 2005. Neoproterozoic paleogeography of the Cadomia and Avalon terranes: constraints from detrital zircon U–Pb ages. Journal of the Geological Society, London 162, 6571.CrossRefGoogle Scholar
Seston, R., Winchester, J. A., Piasecki, M. A. J., Crowley, Q. G. & Floyd, P. A. 2000. A structural model for the western-central Sudetes: a deformed stack of Variscan thrust sheets. Journal of the Geological Society, London 157, 1155–67.CrossRefGoogle Scholar
Teisseyre, H. 1963. Siodło Bolków-Wojcieszów jako charakterystyczny przykład struktury kaledońskiej w Sudetach Zachodnich. The Bolków–Wojcieszów Anticline – a representative Caledonian structure in the Western Sudetes. Prace Instytutu Geologicznego 30, 279300 (in Polish, English summary).Google Scholar
Urbanek, Z. & Baranowski, Z. 1986. Revision of the age of the Radzimowice slates from the Góry Kaczawskie, Western Sudetes. Annales Societas Geologorum Poloniae 56, 399408.Google Scholar
Von Raumer, J. F., Stampfli, G. M. & Bussy, F. 2003. Gondwana-derived microcontinents – the constituents of the Variscan and Alpine collisional orogens. Tectonophysics 365, 722.CrossRefGoogle Scholar
Zimmermann, E. 1932. Geologische Karte von Preussen und benachbarten deutschen Landern, 1:25 000, Blatt Hirschberg. Berlin: Preussische Geologische Landesanstalt.Google Scholar