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New moldavites from SW Poland

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Four newly discovered moldavites from the East and West Gozdnica pits, SW Poland, are characterized. All specimens, including other four, reported earlier, are from Upper Miocene fluvial sediments of the Gozdnica Formation. Their weight varies between 0.529 and 1.196 g. The moldavites are bottle green in colour and have bubbles and inclusions of lechatelierite. Low degree of corrosion suggests short river transport, apparently eastward from Lusatia.
Słowa kluczowe
Rocznik
Strony
99--105
Opis fizyczny
Bibliogr. 46 poz., fot., rys., tab.
Twórcy
  • Department of Geochemistry, Mineralogy and Petrography; Faculty of Earth Science; University of Silesia; Będzińska Str. 60, PL-41-200 Sosnowiec, Poland
autor
  • Department of Geochemistry, Mineralogy and Petrography; Faculty of Earth Science; University of Silesia; Będzińska Str. 60, PL-41-200 Sosnowiec, Poland
  • Department of Geochemistry, Mineralogy and Petrography; Faculty of Earth Science; University of Silesia; Będzińska Str. 60, PL-41-200 Sosnowiec, Poland
Bibliografia
  • 1. Artemieva, N., Pierazzo, E. and Stöffler, D. 2002. Numerical modeling of tektite origin in oblique impacts: Implication to Ries-Moldavites strewn field. Bulletin of the Czech Geological Survey, 77, 303–311.
  • 2. Baraniecka, M.D. 1991. Section Różce against main sections of preglacial deposits in southern Mazowsze. Przegląd Geologiczny , 39, 254–257. [In Polish with English summary]
  • 3. Badura, J. and Przybylski, B. 2004. Evolution of the Late Neogene and Eopleistocene fluvial system in the foreland of the Sudetes Mountains (southwest Poland). Annales Societatis Geologorum Poloniae, 74, 43–61.
  • 4. Baker, G. 1963. Form and sculpture of tektites. In: J.A.O’Keefe (Ed.), Tektites, III, pp. 1–24.University of Chicago Press; Chicago.
  • 5. Barnes, V.E. 1969. Petrology of moldavites.GeochimicaetCosmochimicaActa, 33, 1121–1134.
  • 6. Bouška, V. 1964.Geology and stratigraphy of moldavite occurrences. Geochimica et Cosmochimica Acta, 28, 921–922.
  • 7. Bouška, V., Kadlec, J. and Žak, K. 1999. Moldavite aus dem westlichen und dem nordlichen Teil Bohmen. Staatliches Museum fürMineralogie und Geologie, Dresden, 10, 16–19.
  • 8. Brachaniec, T., Szopa, K. and Karwowski, Ł. 2014. Discovery of the most distal Ries tektites found in Lower Silesia, southwestern Poland. Meteoritics & Planetary Science, 49, 1315–1322.
  • 9. Brachaniec, T., Szopa, K. and Karwowski, Ł. 2015. A new discovery of parautochthonous moldavites in southwestern Poland, Central Europe. Meteoritics & Planetary Science, 50, 1697–1702.
  • 10. Buchner, E. and Schmieder, M. 2009. Multiple fluvial reworking of impact ejecta–A case study from the Ries crater, southern Germany. Meteoritics & Planetary Science, 44, 1051–1060.
  • 11. Buchner, E., Schmieder, M., Schwarz, W.H. and Trieloff, M. 2013. Das Alter des Meteoriten craters Nordlinger Ries – eine Übersicht und kurze Diskussion der neueren Datierungen des Ries impakts. Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 164, 433–445.
  • 12. Chao, E.C.T. 1963. The petrographic and chemical characteristics of tektites.In: J.A.O’Keefe (Ed.), Tektites, III, pp. 51–94.University of Chicago Press; Chicago.
  • 13. Dence, M.R. 1971. Impact melts. Journal of Geophysical Research, 76, 5552–5565.
  • 14. Dyjor, S., Kvacek, Z., Łańcucka-Środoniowa, M., Pyszyński, W., Sadowska, A. and Zastawniak, E. 1992.The younger Tertiary deposits in the Gozdnica region (WS Poland) in the light of recent palaeobotanical research. In: E. Zastawniak (Ed.), Polish Botanical Studies. Polish Academy of Science, 3, 1–133.
  • 15. Dyjor, S., Sadowska, A., Humemel, A., Baranowska-Zarzycka, Z. and Zastawniak, E. 1998. Geological position and flora of the younger Neogene deposits in Lower Silesia. In: A. Sadowska and A. Szynkiewicz (Eds), The 5th European Palaeobotanical and Palynological Conference, pp. 37–54. Cracow.
  • 16. Engelhardt, W. von 1972. Shock produced rock glasses from the Ries crater. Contributions to Mineralogy and Petrology, 36, 265–292.
  • 17. Engelhardt, W. von., Luft, E., Arndt, J., Schock, H. and Weiskirchner, W. 1987. Origin of moldavites. Geochimica et Cosmochimica Acta, 51, 1425–1443.
  • 18. Engelhardt, W. von, Berthold, C., Wenzel, T. and Dehner, T. 2005.Chemistry, small-scale inhomogeneity, and formation of moldavites as condensates from sands vaporized by the Ries impact. Geochimica et Cosmochimica Acta, 69, 5611–5626.
  • 19. Glass, B.P. and Simonson, B.M. 2013. Distal impact ejecta layers. A record of large impacts in sedimentary deposits, pp. 1–716. Springer; Berlin – Heidelberg.
  • 20. Grocholski, A. 1977.The marginal Sudetic fault against the Tertiary volcanotectonics. Prace Geologiczno-Mineralogiczne, 6, 89–103.
  • 21. Jessberger, E. and Gentner, W. 1972. Mass spectrometric analysis of gas inclusions in Muong Nong glass and Libyan Desert Glass. Earth and Planetary Science Letters,14, 221–225.
  • 22. Knobloch, V. 1997. Nektere problemv zniku vltavinu III. – Tvary inkluzi a textura ve svetle impaktoveho procesu, Přirodovědný sborník Západomoravského muzea v Třebíči, 31, 54–60.
  • 23. Knobloch, V., Knoblochová Z. and Urbanec, Z. 1981.Beitragzur Morphologie von Lechatelierit in Moldaviten.Chemie der-Erde, 40, 83–95.
  • 24. Knobloch, V., Knoblochová, Z. and Urbanec, Z. 1983. Struktur und Textur von Lechatelieriteinschlussen und ihre Beziehungen zur Morphologie der Moldavite. Chemie der Erde, 42, 145–154.
  • 25. Koeberl, C. 2007. The geochemistry and cosmochemistry of impacts. In: H.D. Holland and K.K. Turekian (Eds), Meteorites, comets, and planets, pp. 1–52. Elsevier; Oxford.
  • 26. Koeberl, C., Brandstätter, F., Niedemmazr, G. and Kurat, G. 1988. Moldavites from Austria. Meteoritics, 23, 325–332.
  • 27. Kural, S. 1979. Origin, age and geologic background of the kaolin in the western part of the Strzegom. Biuletyn Instytutu Geologicznego, 313, 9–68.
  • 28. Lange, J.M. 1995. Lausitzer Moldavite und ihre Fundschichten, pp. 1–134. Schriften für Geowissenschaften 3; Berlin.
  • 29. Lange J.-M. 1996. Tektite glasses from Lusatia (Lausitz), Germany. Chemie der Erde, 56, 498–510.
  • 30. Magna, T., Deutsch, A., Mezger, K., Skála, R., Seitz, H.M., Mizera, J., Řanda, Z. and Adolph, L. 2011. Lithium in tektites and impact glasses: Implications for sources, histories and large impacts. Geochimica et Cosmochimica Acta, 75, 2137–2158.
  • 31. Meisel, T., Lange, J.-M.andKrahenbuhl, U. 1997. The chemical variation of moldavite tektites: Simple mixing of terrestrial sediments. Meteoritics & Planetary Science, 32, 493–502.
  • 32. Osinski, G.R. 2003. Impact glasses in fallout suevites from the Ries impact structure, Germany: An analytical SEM study. Meteoritics & Planetary Science, 38, 1641–1667.
  • 33. Piwocki, M. and Ziembińska-Tworzydło, M. 1997. Neogene of the Polish Lowlands – lithostratigraphy and pollen-spore zones. Geological Quarterly, 41, 21–40.
  • 34. Piwocki, M., Badura, J. and Przybylski, B. 2004. Neogen: miocen, pliocen. In: T. Peryt and M. Piwocki (Eds), Geologia Polski, 1, 71–201. Państwowy Instytut Geologiczny; Warszwa.
  • 35. Řanda, Z., Mizera, J., Frána, J. and Kučera, J. 2008. Geochemical characterization of moldavites from a new locality, the Cheb Basin, Czech Republic. Meteoritics & Planetary Science, 43, 461–477.
  • 36. Sadowska, A. 1992. A palynological study of the profiles from Gozdnica and Gozdnica-Stanislaw localities. In: E. Zastawniak (Ed.), The younger Tertiary deposits in the Gozdnica region (SW Poland) in the light of recent palaeobotanical research. Polish Botanical Studies, 3, 11–17.
  • 37. Skála, R. and Čada, M. 2003. Major element composition of three moldavites from Dřenice, the Cheb Basin, Czech Republic. Acta Scientiarum Naturalium Musei Moraviae Occidentalis Třebíč, 41, 11–17.
  • 38. Stachurska, A., Dyjor, S., Kordysz, M. and Sadowska, A. 1971. Paleobotanic characteristics of Late Tertiary sediments at Gozdnica (Lower Silesia). Annales de la Société géologique de Pologne, 41, 359–386. [In Polish with English summary]
  • 39. Stöffler, D. 1984. Glasses formed by hypervelocity impact. Journal of Non-Crystalline Solids, 67, 465–502.
  • 40. Stöffler, D., Artemieva, N.A. and Pierazzo, E. 2002. Modeling the Ries-Steinheim impact event and the formation of the moldavite strewn field. Meteoritics & Planetary Science, 37, 1893–1907.
  • 41. Suess, H.E. 1951. Gas content and age of tektites. Geochimica et Cosmochimica Acta, 2, 76–79.
  • 42. Szynkiewicz, A. 2011. Wiek utworów neogenu w Zachodniej części Dolnego Śląska. In: A. Żelaźniewicz, J. Wojewoda and W. Ciężkowski (Eds), Mezozoik i kenozoik Dolnego Śląska, pp. 11–18.WIND.
  • 43. Trnka, M. and Houzar, S. 2002. Moldavites: a review. Bulletin of the Czech Geological Survey, 77, 283–302.
  • 44. Žák, K., Skála, R., Řanda, Z. and Mizera, J. 2012. A review of volatile compounds in tektites, and carbon content and isotopic composition of moldavite glass. Meteoritics & Planetary Science, 47, 1010–1028.
  • 45. Žebera, K. 1972. Vltaviny v katastrofalnich přivalovych sedimentech u Prahy. Geologicky Průzkum, 14, 54–56.
  • 46. Żelaźniewicz, A., Wojewoda, J. and Ciężkowski W. 2011. Przewodnik do wycieczek LXXXI Zjazdu Polskiego Towarzystwa Geologicznego. pp. 1–72. Polskie Towarzystwo Geologiczne; Wrocław
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-5d2e2b50-2b52-4968-b1a3-9d35bee6d17c
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