PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Radiometric dating of the Tertiary volcanics in Lower Silesia, Poland

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Tertiary volcanic rocks of the Fore-Sudetic Block (FSB), Lower Silesia (Poland), exposed between Strzelin in the east and Legnica in the west, typically represent within-plate basalts. Petrologically, they consist mainly of alkali basalts, basanites, tephrites and ankaratrites. 16 new K-Ar dates are recorded, spanning the Oligocene (31 Ma) through Early Miocene (Burdigalian c. 18 Ma) time. The majority of these K-Ar dates plot around two significantly different ages: 27š1.5 Ma, and 20š1.5 Ma. They indicate the presence in the FSB of two distinct separate phases of Tertiary vulcanicity: (i) the first phase, mainly Late Oligocene (Chattian), with a peak at c. 27; (ii) the second phase, Early Miocene (Aquitanian-Burdigalian), with a peak at about 20 Ma. These phases seem to be separated by a gap in vulcanicity about 3 Ma long at the Oligocene/Miocene boundary. Correlation of K-Ar-dated volcanic activity in the FSB with specific radiometrically-dated polarity intervals, poses some problems, and cannot be regarded definite at this stage of investigations. Considering the whole set of K-Ar and palaeomagnetic data from 40 sites, between the Opole area in the east and the Legnica area in the west, we suggest that volcanism of the first phase (Oligocene), although significantly spread out in time across multiple reversals, took place mostly during two well-defined, previously recognized events: (i) an older, reversed Odra event (within the C9r chron: 28.1š1.2 Ma); and (ii) a younger, normal Gracze event (within the C8n chron: 26.5š1.1 Ma). The second phase (Early Miocene) volcanism includes mainly a continuous set of reversely magnetized sites (mostly a single reversed C6r chron: 20.5š0.87 Ma).
Rocznik
Strony
1--19
Opis fizyczny
Bibliogr. 37 poz., rys., tab.
Twórcy
  • Institute of Geological Sciences, Polish Academy of Sciences, Cracow Research Centre, Senacka 1, 31-002 Kraków, Poland
autor
  • Institute of Nuclear Research, Hungarian Academy of Sciences, Bem tér. 18c, 4001 Debrecen, Hungary
autor
  • Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland
autor
  • Institute of Geological Sciences, Polish Academy of Sciences, Sudetic Geology Department, Podwale 75, 50-449 Wrocław
  • Institute of Mining, Wroclaw University of Technology, pi. Teatralny 2, 50-051 Wrocław, Poland
Bibliografia
  • 1. August, Cz., Awdankiewicz, M. & Wojewoda, J., 1995. Tertiary basaltoids, volcanoclastics and sedimentary rocks in the eastern part of the Fore-Sudetic Block (in Polish). In: Geology and environmental protection of the Fore-Sudetic Block. Guide, LXVI Field Meeting of the Geological Society of Poland. Wrocław.
  • 2. Balogh, K., 1986. K-Ar dating of Neogene volcanic activity in Hungary: Experimental technique, experiences, and methods of chronological studies. ATOMK1 Report, D/1: 277-288.
  • 3. Berg, G„ 1930. Die niederschlesischen Basaltvorkommen. Sonder Band, Preussische Geologische Landesanstalt, 5: 65-74.
  • 4. Besse, J. & Courtillot, V., 2002. Apparent and true polar wander and the geometry of the geomagnetic field over last 200 Myr. Journal of Geophysical Research, 107 (B11), EPM 6: 1-31.
  • 5. Birkenmajer, K., 1967. Lower Silesian basalts as monuments of inanimate nature (in Polish, English summary). Rocznik Ochrony Przyrody (Kraków), 32: 225-276.
  • 6. Birkenmajer, K. & Naim, A. E. M., 1969. Palaeomagnetic investigations of the Tertiary and Quaternary igneous rocks. V. The basic Tertiary basalts of Lower Silesia, Poland. Geologische Rundschau, 58: 697-712.
  • 7. Birkenmajer, K. & Pécskay, Z., 1999. K-Ar dating of the Miocene andesite intrusions, Pieniny Mts, West Carpathians. Bulletin of the Polish Academy of Sciences: Earth Sciences, 47: 155-169.
  • 8. Birkenmajer, K. & Pécskay, Z., 2000. K-Ar dating of the Miocene andesite intrusions, Pieniny Mts, West Carpathians, Poland: a supplement. Studia Geologica Polonica, 117: 7-25.
  • 9. Birkenmajer, K. & Pécskay, 2002. Radiometric dating of the Tertiary volcanics in Lower Silesia, Poland. I. Alkali basaltic rocks of the Opole region. Bulletin of the Polish Academy of Sciences, Earth Sciences, 50 (1) 21-40.
  • 10. Birkenmajer, K., Jerzmański, J. & Naim, A. E. M., 1970. Palaeomagnetic studies of Polish rocks. IV. Cenozoic basalts of Lower Silesia. Annales de la Société Géologique de Pologne, 40: 31-61.
  • 11. Birkenmajer, K., Jeleńska, M., Kądziałko-Hofmokl, M. & Kruczyk, J., 1972. Magnetic properties of Polish Tertiary basaltic rocks from the Opole region. Publications, Institute of Geophysics, Polish Academy of Sciences, 57: 59-68.
  • 12. Birkenmajer, K., Jeleńska, M., Kądziałko-Hofmokl, M. & Kruczyk, J., 1977. Age of deep-seated fracture zones in Lower Silesia (Poland), based on K-Ar and palaeomagnetic dating of Tertiary basalts. Annales de la Société Géologique de Pologne, 47: 545-552.
  • 13. Birkenmajer, K., Pécskay, Z., Grabowski, J., Lorenc, M. W. & Za~ gożdżon, P. P., 2002a. Radiometric dating of the Tertiary volcanics in Lower Silesia, Poland. II. K-Ar ages and palaeomagnetic data from Neogene basanites near Lądek Zdrój, Sudetes Mts. Annales Societatis Geologorum Poloniae, 72 (2): 119-129.
  • 14. Birkenmajer, K., Pécskay, Z., Grabowski, J., Lorenc, M. W. & Zagożdżon, P. P., 2002b. Radiometrie dating of the Tertiary volcanics in Lower Silesia, Poland. III. K-Ar ages and palaeomagnetic data from Early Miocene basaltic rocks near Jawor, Fore-Sudetic Block. Annales Societatis Geologorum Poloniae, 72 (3): 241-253.
  • 15. Cande, S. C. & Kent, D. V., 1995. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. Journal of Geophysical Research, 1000: 6093-6095.
  • 16. De la Roche, H., Letterier, J., Grandclaude, P. & Marchal, M., 1980. A classification of volcanic and plutonic rocks using RlR2-diagram and mayor element analysis - its relationship with current nomenclature. Chemical Geology, 29: 183-210.
  • 17. Jerzmański, J., 1956. The basalts in the vicinity of Jawor in Lower Silesia (in Polish, English summary). Biuletyn Instytutu Geologicznego (Warszawa), 106: 119-132.
  • 18. Jerzmański, J., 1961. Comment on the geological structure of the Jawor region in Lower Silesia. Uniwersytet Wrocławski, Zeszyty Naukowe, Ser. B: 8: 113-121.
  • 19. Jerzmański, J., 1965. Geology of the north-western part of the Kaczawa Mountains and of their eastern extent (in Polish, English summary). Biuletyn Instytutu Geologicznego (Warszawa), 185: 109-193.
  • 20. Jerzmański, J. & Maciejewski, S., 1968. Tertiary basalts in Lower Silesia. Biuletyn Instytutu Geologicznego (Warszawa), 227: 247-260.
  • 21. Kirschvink, J. L., 1980. The least square line and plane and the analysis of palaeomagnetic data. Journal of the Royal Astronomical Society, 62: 699-718.
  • 22. Kopecký, L., 1966. Tertiary volcanics, in Svoboda, J. (ed.). Regional Geology of Czechoslovakia. I. The Bohemian Massif. Czechoslovak Academy of Sciences (Praha): 554-581.
  • 23. Kądziałko-Hofmokl, M. & Kruczyk, J., 1976. Complete and partial self-reversal of natural remanent magnetization of basaltic rocks from Lower Silesia. PAGEOPH, 114: 207-213.
  • 24. Kozlowska-Koch, M., 1987. Clasification and nomenclature of the Tertiary volcanic rocks of the Lower and Opole Silesia (in Polish, English summary). Archiwum Mineralogiczne, 42: 43-95.
  • 25. Kruczyk, J., Kądziałko-Hofmokl, M., Jeleńska, M. & Birkenmajer. K., 1977a. Paleomagnetism and magnetic properties of Tertiary basaltic rocks from Góra św. Anny and Ligota Tulowicka, Lower Silesia. Publications, Institute of Geophysics, Polish Academy of Sciences, C3 (111): 1-17.
  • 26. Kruczyk, J., Kądziałko-Hofmokl, M., Jeleńska, M., Birkenmajer, K. & Arakelyants, M. M., 1977b. Tertiary polarity events in Lower Silesian basalts and their K-Ar age. Acta Geophysica Polonica, 25: 183-191.
  • 27. Kural, S., 1982. Explanations to the geological map, 1:25,000 scale, sheet Strzegom (in Polish). Polish Geological Institute (Warsaw).
  • 28. Le Bas, M. J. & Streckeisen, A. L., 1991. The IUGS systematics of igneous rocks. Journal of the Geological Society (London), 148: 825-833.
  • 29. Lewandowski, M., Nowożyński, K. & Werner, T., 1997. PDA - a package of FORTRAN programs for paleomagnetic data analysis. Mscr., Institute of Geophysics, Polish Academy of Sciences (Warsaw).
  • 30. Palmer, A. R. & Geissman, J., 1999. Geologic Time Scale. Geological Society of America. Product code CTS004.
  • 31. Pearce, J. A. & Gale, G. H., 1977. Identification of ore deposition environment from trace element geochemistry of associated igneous rocks. Geological Society (London), Special Publication, 7: 14-24.
  • 32. Śliwa, Z., 1967. Structures in Silesian basalts (in Polish, English summary). Annales de la Société Géologique de Pologne, 37 (3): 435-454,
  • 33. Steiger, R. H. & Jäger, E., 1977. Subcommission on the use of decay constants in Geo- and Cosmochronology. Earth and Planetary Science Letters, 36: 359-362.
  • 34. Torsvik, T. H., Mosar, J. & Eide, E. A., 2001. Cretaceous-Tertiary dynamics: a North Atlantic exercise. Geophysical Journal International, 146: 850-866.
  • 35. Wójcik, L., 1973. Explanations to geological map of the Sudeten Mts, 1:25,000 scale, Ciepłowody sheet. Geological Institute (Warsaw).
  • 36. Wojno, T., Pentlakowa, Z. & Szarras, S., 1951. Investigations of Lower Silesian basalts in the years 1950-1951 (in Polish, unpublished). Państwowy Instytut Geologiczny, Archiwum (Warszawa).
  • 37. Zagożdżon, P. P., 2001. “Sunburn” (“Sonnenbrand”) in Tertiary basalts of Lower Silesia and possibilities of utilizing them (in Polish). Ph.D. Thesis.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS7-0003-0014
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.