Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
New palaeomagnetic poles obtained from the Vendian tuffs and basalts of western Ukraine indicate the necessity of a substantial revision of the Late Vendian-Early Cambrian palaeogeography of the Baltic plate. The palaeopole calculated for the most stable component isolated from the Vendian tuffs and basalts is far away from the Vendian-Cambrian apparent polar wander path (APWP), constructed on the basis of Scandinavian poles but is very close to the pole recently isolated from the Vendian sediments of the White Sea Region. Depending on the polarity of the newly-determined Late Vendian pole, two palaeogeographic models of the Baltic plate in the Late Vendian-Early Cambrian are possible. In our preferred model the Baltic plate moved at that time from the moderate southern latitudes to the equator rotating anticlockwise of ca. 120 degrees Celsius. This reconstruction explains the geological structures of the marginal zones of Baltica better than the previously proposed stationary model of the Late Vendian-Cambrian Baltica. According to the new late Vendian palaeogeographic scenario, the European, passive margin of Baltica was separated from an active, Avalonian margin of Gondwana. The Late Neoproterozoic tectonic structures of the Brunovistulian Terrane and the Małopolska Block were developed near the present day southwestern corner of Baltica that was tectonically active at that time. Alternative reconstruction shows the Baltic platemoving from the moderate northern latitudes in the Vendian, crossing palaeoequator in the latest Vendian, and reaching moderate southern palaeolatitudes in the Late Cambrian. This model, however, would have required exceptionally high plate velocity (ca. 33 cm/year).
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
309--316
Opis fizyczny
Bibliogr. 44 poz., rys.
Twórcy
autor
- Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland
autor
- Deptartment of Geography, Lvov University, Doroszenki 41, 290000 Lvov, Ukraine
autor
- Institute of Geology and Geography, Ševčenkos St. 13, LT-2600 Vilnius, Lithuania
Bibliografia
- 1. BIAŁOWOLSKA A., BAKUN-CZUBAROW N. and FEDORYSHYN Y. (2002) - Neoproterozoic flood basalts of the upper beds of the Volhynian Series (East European Craton). Geol. Quart., 46 (1): 37-58.
- 2. BROCHWICZ-LEWIŃSKI W., VIDAL G., POŻARYSKI W., TOMCZYK H. and ZAJĄC R. (1986) - Pre-Permian tectonic position of the Upper Silesian Massif (S Poland) in the light of studies on the Cambrian. C. R. Acad. Sc. Paris, 303, II (16): 1493-1496.
- 3. BUCHAN K. L. and HALLS H. C. (1990) - Paleomagnetism of Proterozoic mafic dyke swarms of the Canadian Shield. In: Mafic Dykes and Emplacement Mechanism (ed. A. J. Parker, P. C. Rickwood and D. H. Tucker): 209-230. A. A. Balkema Rotterdam.
- 4. COMPSTON W., SAMBRIDGE M. S., REINFRANK R. F., MOCZYDŁOWSKA M., VIDAL G. and CLAESSON S. (1995) - Numerical ages of volcanic rocks and the earliest faunal zone within the Late Precambrian of east Poland. J. Geol. Soc., London, 152: 599-611.
- 5. DADLEZ R. (1995) - Debates about pre-Variscan tectonics of Poland. Stud. Geophys. Geodet., 39: 227-234.
- 6. DUDEK A. (1980) - The crystalline basement block of the outer Carpathians in Moravia: Bruno-Vistulicum. Rozpr. Ceskoslov. Akad. Ved, 90 (8): 81-85.
- 7. FINGER F., HANZL P., PIN C., VON QUADT A. and STEYRER H. P. (2000) - The Brunovistulian: Avalonian Precambrian sequence at the eastern end of the Central European Variscides ? In: Orogenic Processes, Quantification and Modelling in the Variscan Belt (eds. W. Franke, V. Haak, O. Oncken and D. Tanner). Geol. Soc. London, Spec. Pub., 179: 103-112.
- 8. FISHER R. A. (1953) - Dispersion on a sphere. Proc. R. Soc. London Ser. A 217: 295-305.
- 9. FRANKE D. (1995) - Caledonian terranes along the southwestern border of the East European Platform - evidence, speculation and open questions. Stud. Geophys. Geodet., 39: 241-256.
- 10. GLASMACHER U. A., GIESE U., STROINK L., REYNOLDS P., ALEKSEYEV A., PUCHKOV V. and BAUER W. (1999) - Neoproterozoic terrane at the eastern margin of Baltica - implications for Late Proterozoic palaeogeography and structural evolution of SW Urals, Russia. EUG10 J. Conference Abstracts.
- 11. HARTZ E. and TORSVIK T. H. (2002) - Baltica upside down: a new plate tectonic model for Rodinia and the Iapetus Ocean. Geology, 30: 255-258.
- 12. HEGNER E. and KRÖNER A. (2000) - Reviev of Nd isotopic data and xenocrystic and detrital zircon ages from the pre-Variscan basement in the eastern Bohemian Massif: speculations on palinspastic reconstructions. In: Orogenic Processes, Quantification and Modelling in the Variscan Belt (eds. W. Franke, V. Haak, O. Oncken and D. Tanner). Geol. Soc. London, Spec. Pub., 179: 113-130.
- 13. JAWOROWSKIK. and SIKORSKA M. (2003) - Composition and provenance of clastic material in the Vendian-lowermost Cambrian from northern Poland: Geotectonic implications. Państ. Inst.Geol., Spec. Pap., 8: 1-60.
- 14. KALVODA J., MELICHAR R., BABEK O. and LEICHMANN J. (2002) - Late Proterozoic-Paleozoic tectonostratigraphic development and paleogeography of Brunovistulian Terrane and comparision with other terranes at the SE margins of Baltica-Laurussia. J. Czech Geol. Soc., 47 (3-4): 32-41.
- 15. KALVODA J., LEICHMANN J., BABEK O. and MELICHAR R. (2003) - Brunovistulian terrane (Central Europe) and Istanbul zone (NW Turkey): late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography. Geol. Carpath., 54 (3): 139-152.
- 16. KIRSCHVINK J. L. (1980) - The least square line and plane and the analysis of paleomagnetic data, Geophys. J. R. Astron. Soc., 62: 699-718.
- 17. KOZŁOWSKI W., DOMAŃSKA J., NAWROCKI J. and PECSKAY Z. (2004) - The provenance of the Upper Silurian greywackes from the Holy Cross Mountains (Central Poland). Miner. Soc. Pol. Spec. Papers, 24:251-254.
- 18. LEWANDOWSKI M. (1993) - Paleomagnetism of the Paleozoic rocks of the Holy Cross Mts (Central Poland) and the orgin of the Variscan orogen. Pub. Inst. Geophys. Pol. Acad. Sc., A-23 (265).
- 19. LEWANDOWSKI M. and ABRAHAMSEN N. (2003) - Paleomagnetic results from the Cambrian and Ordovician sediments of Bornholm (Denmark) and Southern Sweden and paleogeographical implications for Baltica. J. Geoph. Res., 108, (B11) EPM3: 1-17.
- 20. MEERT J. G., TORSVIK T. H., EIDE E. A. and DAHLGREN S. (1998) - Tectonic significance of the Fen Province, S. Norway: constrains from geochronology and paleomagnetism. J. Geol., 106: 553-564.
- 21. NARKIEWICZ M. (2002) - Ordovician through earliest Devonian development of the Holy Cross Mts. (Poland): constraints from susbsidence analysis and thermal maturity data. Geol. Quart., 46 (3): 255-266.
- 22. NAWROCKI J. (2000) - Late Silurian paleomagnetic pole from the Holy Cross Mountains: constraints for the post-Caledonian tectonic activity of the Trans-European Suture Zone. Earth Planet. Sc. Lett., 179: 325-334.
- 23. NAWROCKI J., ŻYLIŃSKA A., BUŁA Z., GRABOWSKI J., KRZYWIEC P. and POPRAWA P. (2004) - Early Cambrian location and affinities of the Brunovistulian terrane (Central Europe) in the light of paleomagnetic data. J. Geol. Soc., London, 161: 513-522.
- 24. ORŁOWSKI S. (1985) - Lower Cambrian and its trilobites in the Holy Cross Mts. Acta Geol. Pol., 35 (3-4): 231-250.
- 25. PAJCHLOWA M. and MIŁACZEWSKI L.(1974) - Dewon dolny. In: Atlas litologiczno-paleogeograficzny obszarów platformowych Polski. Cz. I. Proterozoik i paleozoik (eds. J. Czermiński and M. Pajchlowa). Wyd. Geol.
- 26. PASKEVICIUS J. (1997) - The geology of the Baltic Republics. Liet. Geol. Tarnyb., Vilnius.
- 27. PIPER J. D. A. (1988) - Paleomagnetism of late Vendian-earliest Cambrian minor alkaline intrusions, Fen Complex, southeast Norway. Earth Planet. Sc. Lett., 90: 422-430.
- 28. PHARAOH T. C. (1999) - Palaeozoic terranes and their lithospheric boundaries within the Trans-European Suture Zone (TESZ): a review. Tectonophyscis, 314: 17-41.
- 29. POPOV V., IOSIFIDI A., KHRAMOV A., TAIT J. and BACHTADSE V. (2002) - Paleomagnetism of Upper Vendian sediments from the Winter Coast, White Sea region, Russia: implications for the paleogeography of Baltica during Neoproterozoic times. J. Geophys. Res., 107 (B11) EPM 10: 1-8.
- 30. POPRAWA P., ŠLIAUPA S., STEPHENSON R. A. and LAZAUSKIENE J. (1999) - Late Vendian-Early Palaeozoic tectonic evolution of the Baltic basin: regional implications from subsidence analysis. Tectonophysics, 314: 219-239.
- 31. POPRAWA P. and PACZEŚNA J. (2002) - Late Neoproterozoic to Early Paleozoic development of a rift at the Lublin-Podlasie slope of the East European Craton - analysis of subsidence and facies record (in Polish with English summary). Prz. Geol., 50 (1): 49-63.
- 32. POŻARYSKI W. (1991) - The strike-slip terrane model for the North German-Polish Caledonides. Pub. Instit. Geophys., Pol. Acad. Sc., A-19: 3-15.
- 33. ROBERTS and SIEDLECKA (2002) - Timanian orogenic deformations along the northeastern margin of Baltica, Nortwest Russia and Northeast Norway, and Avalonian-Cadomian connections. Tectonophysics, 352: 169-184.
- 34. SCARROW J. H., PEASE V., FLEUTELOT C. and DUSHIN V. (2001) - The late neoproterozoic enganepe ophiolite, Polar Urals, Russia: an extension of the Cadomian arc ? Precambrian Res., 110: 255-275.
- 35. SVENNINGSEN O. M. (1995) - Extensional deformation along the late Precambrian-Cambrian Baltoscandian passive margin: the Sarektjakka Nappe, Swedish Caledonides. Geol. Rundschau, 84: 649-664.
- 36. TORSVIK T. H., SMETHURST M. A., BRIDEN J. C. and STURT B. A. (1990) - A review of Paleozoic paleomagnetic data from Europe and their paleogeographic implications. In: Paleogeography and Biogeography (eds. W. S. McKerrow and C. R. Scotese): 25-41. Geol. Soc., London, Spec. Pub.
- 37. TORSVIK T. H. and REHNSTRÖM E. F. (2001) - Cambrian palaeomagnetic data from Baltica: implications for true polar wander and Cambrian palaeogeography. J. Geol. Soc., London, 158: 321-329.
- 38. TORSVIK T. H., SMETHURST M. A., MEERT J. G., VAN DER VOO R., MC KERROW W. S., BRASIER M. D., STURT B. A. and WALDERHAUG H. J. (1996) - Continental break-up and collision in the Neoproterozoic and Paleozoic - a tale of Baltica and Laurentia. Earth Sc. Rev., 40: 229-258.
- 39. VALVERDE-VAQUERO P., DÖRR W., BELKA Z., FRANKE W., WISZNIEWSKA J. and SCHASTOK J. (2000) - U-Pb single-grain dating of detrital zircon in the Cambrian of central Poland: implications for Gondwana versus Baltica provenance studies. Earth Planet. Sc. Let., 184: 225-240.
- 40. VAN BREEMEN O., AFTALION M., BOWES D. R., DUDEK A., MISAR Z., POVONDRA P. and VRANA S. (1982) - Geochronological studies ofthe Bohemian Massif, Czechoslovakia, and their significance in the evolution of Central Europe. Transact. Royal Soc. Edinburgh: Earth Sc., 73: 89-108.
- 41. WILLNER A. P., ERMOLAEVA T., STROINK L., GLASMACHERU. A., GIESEU., PUCHKOV V. N., KOZLOV V. I. and WALTER R. (2001) - Contrasting provenance signals in Riphean and Vendian sandstones in the SW Urals (Russia): constraints for a change from passive to active continental margin conditions in the Neoproterozoic. Precambrian Res., 110:215-239.
- 42. ZIJDERVELD J. D. A. (1967) - AC demagnetization of rocks: analysis of results. In: Methods in Paleomagnetism (eds. D. W. Collinson et al.): 254-287. New York, Elsevier.
- 43. ŻELAŹNIEWICZ A. (1998) - Rodinian-Baltican link of the Neoproterozoic orogen in southern Poland. Acta Univ. Carolinae, Geol., 42: 509-511.
- 44. ŻELAŹNIEWICZ A., SEGHEDI A., JACHOWICZ M., BOBIŃSKI W., BUŁA Z. and CWOJDZIŃSKI S. (2001) - U-Pb SHRIMP data confirm the presence of a Vendian Foreland Flysch Basin next to the East European Craton. ESF Europrobe Meeting “Neoproterozoic-Early Palaeozoic Time-Slice Symposium: Orogeny and Cratonic Response on the Margins of Baltica”, Ankara, Abstracts: 98-100.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT3-0016-0052