Alleged Caboniferous (Viséan) volcanism at the eastern margin of the Moravo-Silesian Basin, Kraków region, Southern Poland

• Autorzy: Lewandowska A. , Rospondek M. J. , Kobuszewski Ł.

Identyfikatory

DOI

10.14241/asgp.2018.005

• Języki publikacji: EN

Abstrakty

EN

The volcanic rocks, represented by clasts in the breccias occurring within the Viséan Culm sequence at Głuchówki, previously were considered to provide evidence of the earliest record of Variscan volcanism on the eastern margin of Moravo-Silesian Basin in the Kraków area. The breccias have been described as the deposits of submarine slides, accompanying the Viséan volcanic activity. This paper provides evidence of a different mode of origin. The present study, based on new field observations, combined with petrological and geochemical data, showed that volcanic rocks are major framework constituents of a breccia and are accompanied by clasts of spotty hornfels and Culm mudstone. Some clasts originated in erosion of the nearby Permian Zalas rhyodacite laccolith and the spotty hornfelses of the contact aureole, while other clasts came from the Culm mudstones. The breccia framework components are not rounded and poorly rounded, which reflects their short distance of transport. Therefore, an alternative scenario for the genesis of the breccia is proposed. The breccias represent material deposited in erosional pockets formed along the bedding of the Culm mudstones. The red iron oxide shells around clasts may indicate weathering in a warm continental climate, thus constraining the breccia formation to either the Permian or the Early or Late Triassic. Thus, the only well documented Viséan igneous rock in the study area remains the diabase, known from the Klucze borehole. Conversely, no volcanic rocks of this age have been documented in the area under consideration.

Słowa kluczowe

EN

Viséan volcanism; Culm; rhyodacite; breccias; Zalas laccolith

• Wydawca: Polskie Towarzystwo Geologiczne
• Czasopismo: Annales Societatis Geologorum Poloniae
• Rocznik: 2018
• Tom: Vol. 88, No. 1
• Strony: 59--69
• Opis fizyczny: Bibliogr. 52 poz., rys, tab., wykr.

Twórcy

autor

Lewandowska A.

• Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387, Kraków, Poland

autor

Rospondek M. J.

• Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387, Kraków, Poland

autor

Kobuszewski Ł.

• Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387, Kraków, Poland

Bibliografia

• 1. Appelt, J., 1998. Tournaisian conodonts from the basinal carbonates of the Krzeszowice area, southern Poland. Acta Geologica Polonica, 48: 135-140.
• 2. Awdankiewicz, M., 1999. Volcanism in a late Variscan intramontane trough: Carboniferous and Permian volcanic centres of the Intra-Sudetic Basin, SW Poland. Geologia Sudetica, 32: 13-47.
• 3. Awdankiewicz, M., Kryza, R. & Szczepara, N., 2013. Timing of post-collisional volcanism in the eastern part of the Variscan Belt: constrains from SHRIMP zircon dating of Permian rhyolites in the North-Sudetic Basin (SW Poland). Geological Magazine, 151: 611-628.
• 4. Bogacz, K., 1980. Tectonics of the Palaeozoic rocks of the Dębnik region. Rocznik Polskiego Towarzystwa Geologicznego, 50: 183-208. [In Polish, with English summary.]
• 5. Bełka, Z., 1982. Upper Viésean conodonts from Głuchówki in the Cracow Upland: stratigraphical and paleothermal implications. Acta Geologica Polonica, 32: 57-67.
• 6. Czarniecki, S., 1955. Lower Carboniferous fauna in the Culm facies of the eastern Upper Silesian Coal Basin. Bulletin de 1’Academie Polonaise des Sciences, 3: 461-464.
• 7. Czarniecki, S. & Łydka, K., 1958. Lower Carboniferous volcanism in the Krzeszowice area. Acta Geologica Polonica, 8: 501-514. [In Polish, with English summary.]
• 8. Czarniecki, S. & Łydka, K., 1962. On the petrographic character of pebbles from volcanic rocks in Lower Carboniferous deposits near Zalas. Acta Geologica Polonica, l12: 335-338. [In Polish, with English summary.]
• 9. Czerny, J. & Muszyński, M., 1997. Co-magmatism of the Permian volcanites of the Krzeszowice Area in the light of petrochemical data. Mineralogia Polonica, 28: 3-25.
• 10. Doktorowicz-Hrebnicki, S., 1955. Mapa geologiczna Górnośląskiego Zagłębia Węglowego. Mapa bez utworów czwartorzędowych. Skala 1:50000, arkusz Alwernia. Wydawnictwo Geologiczne, Warszawa. [In Polish.]
• 11. Dvořák, J., 1973. Synsedimentary tectonics of the Paleozoic of the Drahany Upland (Sudeticum, Moravia, Czechoslovakia). Tectonophysics, 17: 359-391.
• 12. Dzik, J., 1984. Phylogeny of the Nautiloidea. Palaeontologia Polonica, 45: 3-219.
• 13. Dżułyński, S., 1955. On the geological form on the porphyry in the Vicinity of Zalas. Biuletyn Instytutu Geologicznego, 97: 9-33. [In Polish, with English summary.]
• 14. Eisele, J., Gertisser, R. & Montenari, M., 2000. Geochemistry and provenance of Devono-Carboniferous volcano sedimentary sequence from the Southern Vosges Basin and the geodynamic implications for the western Moldanubian Zone. In: Franke, W., Haak, V., Oncken, O. & Tanner, D. (eds), Orogenic Processes: Quantification and Modelling in the Variscan Belt. Geological Society Special Publication, 179, pp. 35-61.
• 15. Gradziński, R., 2009. Geological Map of Cracow Region. Geological Museum, Polish Academy of Sciences, Kraków.
• 16. Grocholski, A. & Ryka, W., 1995. Carboniferous magmatism of Poland. In: Zdanowski, A. & Ryka, W. (eds), The Carboniferous system in Poland. Prace Państwowego Instytutu Geologicznego, 148: 181-189.
• 17. Gromczakiewicz-Łomnicka, A., 1972. Viséan gastropods from Głuchówki near Cracow. Prace Muzeum Ziemi, 20: 3-44.
• 18. Gromczakiewicz-Łomnicka, A., 1974. Upper Viséan conodont fauna from the Carboniferous limestone north of Krzeszowice (environs of Cracow, Poland). Annales de la Société Géologique de Pologne, 44: 475-482.
• 19. 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.
• 20. Harańczyk, C., 1985. Mineral parageneses of Cracovides and its cover (Southern Poland). Annales Societatis Geologorum Poloniae, 53: 91-126.
• 21. Harańczyk, C., 1989a. Rozwój wulkanizmu krakowskiego. In: Rutkowski, J. (ed.), Przewodnik LX Zjazdu Polskiego Towarzystwa Geologicznego. Wydawnictwa AGH, Kraków, pp. 51-58. [In Polish.]
• 22. Harańczyk, C., 1989b. Kominy wulkaniczne Zalasu. In: Rutkowski, J. (ed.), Przewodnik LX Zjazdu Polskiego Towarzystwa Geologicznego. Wydawnictwa AGH, Kraków, pp. 61-67. [In Polish.]
• 23. Hoffmann, M., Paszkowski, M., Uchman, F. & Szulc, J., 2009. Stop 2. Orlej Quarry. In: Haczewski, G. (ed.), Abstracts and Field Guide. Facies Succession and its Controls on the Upper Devonian-Lower Carboniferous Carbonate Platform of the Kraków Upland. Sediment 2009, 6th Annual Conference of SEPM-CES Sediment 2009, Kraków, 24-25th June, 2009. Polish Geological Institute, Warszawa, pp. 49-81.
• 24. Kalvoda, J., Babek, O., Fatka, O., Leichmann, J., Melichar, R., Nehyba, S. & Špaček, P., 2008. Brunovistulian terrane (Bohemian Massif, Central Europe) from late Proterozoic to late Paleozoic: a review. International Journal of Earth Sciences, 97: 497-518.
• 25. Kulicka, R. & Nowiński, A., 1978. Sutherlandia stasinskae sp. n. (Tabulata) from the Upper Viséan of Poland. Acta Palaeontologica Polonica, 23: 107-112.
• 26. Kumpera, O. & Martinec, P., 1995. The development of the Carboniferous accretionary wedge in the Moravian-Silesian Paleozoic Basin. Journal of Czech Geological Society, 40: 47-60.
• 27. Lewandowska, A., Banaś, M. & Zygoń, K., 2007. K-Ar dating of amphiboles from andesite of complex dyke in Dubie (southern Poland). Geochronometria, 27: 11-15.
• 28. Lewandowska, A. & Rospondek, M., 2003. Geochemistry of volcanics of the Zalas area near Kraków, South Poland. Polish Mineralogical Society Special Papers, 23: 119-121.
• 29. Lewandowska, A., Rospondek, M. J. & Nawrocki, J., 2009. The geochemistry of volcaniclastic rocks associated with basaltic trachyandesites in the Nieporaz-Brodła graben near Kraków, Southern Poland. In: Lewandowska, A. & Rospondek, M. J. (eds), Permo-Carboniferous volcanism of the Kraków region. Mineralogia, Special Papers, 34: 15-16.
• 30. Lewandowska, A., Rospondek, M. J. & Nawrocki, J., 2010. Stephanian-Early Permian intermediate volcanic rocks from the Nieporaz-Brodla and Sławków grabens near Kraków, Southern Poland. Annales Societatis Geologorum Poloniae, 80: 227-251.
• 31. Muszyński, M., 1995. Systematic position of igneous rocks from the northern margin of the Upper Silesian Coal Basin. Mineralogia Polonica, 26: 33-49.
• 32. Nawrocki, J., Fanning, M., Lewandowska, A., Polechońska, O. & Werner, T., 2008. Palaeomagnetism and the age of the Cracow volcanic rocks (S Poland). Geophysical Journal International, 174: 475-488.
• 33. Nawrocki, J., Krzemiński, L. & Pańczyk, M., 2010. 40Ar-39Ar ages of selected rocks and minerals from the Kraków-Lubliniec Fault Zone, and their relation to the Paleozoic structural evolution of the Malopolska and Brunovistulian terranes (S Poland). Geological Quarterly, 54: 289-300.
• 34. Nawrocki, J., Lewandowska, A. & Fanning, M., 2007. Isotope and paleomagnetic ages of the Zalas rhyodacites (S Poland). Przegląd Geologiczny, 55: 476-478. [In Polish, with English summary.]
• 35. Nowiński, A., 1976. Tabulata and Chaetetida from the Devonian and Carboniferous of southern Poland. Palaeontologia Polonica, 35: 7-108.
• 36. Olempska, E., 1993. An ostracod assemblage from late Viséan shales of the Cracow area. Acta Palaeontologica Polonica, 38: 93-107.
• 37. Osmólska, H., 1970. Revision of non-cyrtosymbolinid trilobites from the Tournaisian-Namurian of Eurasia. Palaeontologia Polonica, 23: 5-165.
• 38. Paszkowski, M., 1995. Description of stops - Cracow region. Stop 2. Orlej Quarry. In: Kumpera, O., Paszkowski, M. & Wajsprych, B. (eds), Transition of the Early Carboniferous pelagic sedimentation into orogenic flysch. An example from the Silesian-Moravian Zone and adjacent areas. XIII International Congress on Carboniferous-Permian, August 28-September 2, 1995. Excursion B-2 Guidebook, Polish Geological Institute, Warszawa, pp. 15-16.
• 39. Piłat, T., 1957. Porphyric pebbles from the shales of the upper Visean of the Region of Zalas (Cracow Region). Biuletyn Instytutu Geologicznego, 115: 167-185. [In Polish, with English summary.]
• 40. Piłat, T., 1960. Krzeszowic Quelques remarquessur les volcanisme intra-carbonifére aux environs de Krzeszowice. Acta Geologica Polonica, 10: 475-484. [In Polish, with French summary.]
• 41. Schaltegger, U., Schneider, J., Maurin, J. & Corfu, F., 1996. Precise U-Pb chronometry of 245-340 Ma old magmatism related to synconvergence extension in the Southern Vosges (Central Variscan Belt). Earth and Planetary Sciences Letters, 144: 403-419.
• 42. Siedlecki, S., 1954. Przewodnik wycieczki w okolice Krzeszowic i Chrzanowa XXVII Zjazdu Polskiego Towarzystwa Geologicznego. Rocznik Polskiego Towarzystwa Geologicznego, 24: 449-462. [In Polish.]
• 43. Słaby, E., 1987. Adularization of plagioclases with accompanying processes in rhyodacites from Zalas near Cracow. Archiwum Mineralogiczne, 42: 69-91.
• 44. Słaby, E., Breitkreuz, C., Żaba, J., Domańska-Siuda, J., Gaidzik, K., Falenty, K. & Falenty, A., 2010. Magma generation in an alternating transtensional-transpressional regime, the Kraków-Lubliniec Fault Zone, Poland. Lithos, 119: 251-268.
• 45. Špaček, P. & Kalvoda, J., 2000. Reconstruction of syn- and post- sedimentary tectonic events in flysch basin from limestone pebbles variation: Drahany Culm of the Moravian Rhenohercynian Zone. Geologica Carpathica, 51: 37-48.
• 46. Timmerman, M. J., 2004. Timing, geodynamic setting and character of Permo-Carboniferous magmatism in the foreland of the Variscan Orogen, NW Europe. In: Wilson, M., Neumann, E.-R., Davies, G. R., Timmerman, M. J., Heeremans, M. & Larsen, B. T. (eds), Permo-Carboniferous Magmatism and Rifting in Europe. Geological Society, London, Special Publications, 223: 41-74.
• 47. Unrug, R., 1977. Lower Carboniferous Flysch in the Głubczyce region (Lower Silesia). Rocznik Polskiego Towarzystwa Geologicznego, 47: 73-92.
• 48. Winchester, J. A. & Floyd, P. A., 1977. Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology, 20: 325-343.
• 49. Wolska, A., 2012. Petrology and geochemistry of granitoids and their mafic micogranular enclaves (MME) in marginal part of the Małopolska Block (S Poland). Mineralogia, 43: 3-127.
• 50. Zachovalová, K. & Leichmann, J., 2003. Clasts of Volcanic rocks from Viséan conglomerates in the Drahany Culm: evidence for a volcanic arc on the eastern margin of Bohemian Massif. Journal of the Czech Geological Society, 48: 139.
• 51. Żaba, J., 1999. Structural evolution of Lower Palaeozoic succession in the Upper Silesia block and Małopolska block zone. Prace Państwowego Instytutu Geologicznego, 16: 5-162.
• 52. Żelaźniewicz, A., Pańczyk, M., Nawrocki, J. & Fanning, M., 2008. A Carboniferous/Permian, calc-alkaline, I-type granodiorite from the Małopolska Block, Southern Poland: implications from geo chemical and U-Pb zircon age data. Geological Quarterly, 52: 301-308.

Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).