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Jeszcze raz o terranach w Polsce i ich wędrówce

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EN
Once again about terranes in Poland and their wandering
Języki publikacji
PL
Abstrakty
EN
Results of interdisciplinary studies conducted until now lead to a univocal conclusion that Poland should be regarded as a collage of terranes of different ages and provenances of the basement, and different amalgamation and accretion scenarios. Geophysical and tectonic-structural investigations have allowed defining, with different accuracies, the boundaries between particular terranes. Terranes located in the area of Paleozoic platform were subjected to two or three phases of mobility. The first phase of transcontinental scale was manifested by large-scale tectonic transport during rebuilding of global paleogeography. The second mobility phase of regional scaleaffected the Teisseyre-Tornquist terrane assemblage and was linked with the Laurentia and Avalonia collision. This process put in motion the escape tectonics in the earliest Devonian. As its result, some of terranes were reshuffled during their tectonic transportation in the SE direction. The third, Carboniferous phase of mobility of only local scale was related mainly to the dextral strike-slip tectonic activity. Unfortunately, in the case of several tectonostratigraphic units, an answer to the questions concerning their initial location and way of migration is still impossible. It is valid also in the case of the Teisseyre-Tornquist terrane assemblage, now located to the SE of the Moravia and Grójec fault zones. This reticence in geological diagnosis occurs in spite of generally good access to the rocks of the Brunovistulia and Małopolska terranes that could contain substantial information about the earliest stages of evolution of these units. In order to eliminate numerous gaps in our knowledge about the Polish terranes a new interdisciplinary scientific program should be developed.
Rocznik
Strony
1272--1283
Opis fizyczny
Bibliogr. 127 poz., rys., tab., wykr.
Twórcy
autor
  • Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy, ul. Rakowiecka 4, 00-975 Warszawa
Bibliografia
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  • 85. MOCZYDŁOWSKA M. 1997 - Proterozoic and Cambrian successions in Upper Silesia: an Avalonian terrane in Southern Poland. Geol. Mag., 134: 679-689.
  • 86. NARKIEWICZ M. 2002 - Ordovician through earliest Devonian development of the Holy Cross Mts. (Poland): Constraints from subsidence analysis and thermal maturity data. Geol. Quart., 46 (3): 255-266.
  • 87. NARKIEWICZ M., GRAD M., GUTERCH A. & JANIK T. 2011 - Crustal seismic velocity structure of southern Poland: Preserved memory of a pre-Devonian terrane accretion at the East European Platform margin. Geol. Mag., 148: 191-210.
  • 88. 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. Sci. Let., 179: 325-334.
  • 89. NAWROCKI J. & POPRAWA P. 2006 - Development of Trans-European Suture Zone in Poland: from Ediacaran rifting to Early Palaeozoic accretion. Geol. Quart., 50: 59-76.
  • 90. NAWROCKI, J., BOGUCKIJ, A. & KATINAS, V. 2004a. New Late Vendian palaeogeography of Baltica and the TESZ. Geol. Quart., 48 : 309-316.
  • 91. NAWROCKI J., ŻYLIŃSKA A., BUŁAZ., GRABOWSKI J., KRZYWIEC P. & POPRAWA P. 2004b - Early Cambrian location and affinities of the Brunovistulian terrane (Central Europe) in the light of palaeomagnetic data. J. Geol. Soc., London, 161: 513-522.
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