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The lower-middle Upper Triassic succession of the Fatricum domain from the Tatra Mts is commonly called the Carpathian Keuper. During Late Triassic, the Fatricum Basin was a proximal part of the central Inner Carpathian Basin. In early Carnian times, carbonate sedimentation stopped. Emersion of the Middle Triassic carbonate platform resulted in development of palaeokarst and pedogenic fabrics and deposition of conglomerates. Typical Carpathian Keuper sediments – variegated shales with intercalations of sandstones and dolomites represent mixed continental/shallow marine environments. Variegated mudstones with pedogenic carbonate concretions and intercalations of thin sandstone beds originated in mudflat environment under the semi-arid climate condition. Thick-bedded, cross-stratified sandstones with common plant debris represent fluvial deposits. They were deposited during the periods of climate pluvialisation. According to ?13C and ?18O data, thick, continuous dolomitic sediments containing local cherts represent marine sediments of perilittoral environments, which were commonly emerged as evidenced by common palaeokarst and palaeosols featuring these complexes. Cyclicity in the lower part of the Carpathian Keuper resulted from climatic changes, whereas dolomite-clastic cycles from the upper part of the succession were generated probably by sea level fluctuations. Moreover, deposition of the Keuper succession was controlled by synsedimentary tectonic which resulted in big facies variability.
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1--18
Opis fizyczny
bibliogr. 56 poz., rys., tab., wykr.
Twórcy
autor
- Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, rychlin@ing.uj.edu.pl
Bibliografia
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- Al-Juboury, A. J. & Durović, V., 1996. Supratidal originof Carpathian Keuper dolostones. Mineralia Slovaca, 28: 12-20.
- Allan, J. R. & Matthews, R. K., 1982. Isotope signatures associated with early meteoric diagenesis. Sedimentology, 29: 797-817.
- Andrusov, D., 1959. Prehlad stratygrafie a tektoniky druhohô-rného pásma masívu Vysokých Tatier na území Slovenska. (In Slovak). Geologický Sbornik Slovenskiej Akademie Vied, 10: 97-127.
- Andrusov, D., Bystrický, J. & Fusán, O., 1973. Outline of the structure of the West Carpathians. X Congress of Carpathian-Balkan Geological Association. Introductory Excursion Guidebook. Geologický Ústav Dionýza Štúra, Bratislava, 45 pp.
- Bac-Moszaszwili , M., 1998. Geology of the Subtatric Units, Western Tatra Mountains, Poland. Studia Geologica Polonica, 111: 113-136.
- Bac-Moszaszwili, M., Burchart, J., Głazek, J., Iwanow, A., Jaroszewski, W., Kotański, Z., Lefeld, J., Mastella, L., Ozimkowski, W., Roniewicz, P., Skupiński, A., Westwalewicz-Mogilska, E., 1979. Geological Map of the Polish Tatra, 1:30 000. Wydawnictwa Geologiczne, Warszawa.
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- Bridges, P. H. & Leeder, M. R., 1976. Sedimentary model for intertidal mudflat channels, with examples from the Solway Firth, Scotland. Sedimentology, 23: 533-552.
- Chafetz, H. S., Imerito-Tetzlaff, A. A. & Zhang, J., 1999. Stable isotopes and elements trends in Pleistocene sabkha dolomites: descending meteoric waters vs. sulfate reduction. Journal of Sedimentary Research, 69: 256-266.
- El-Sayed, M. I., Fairchild, I. J. & Spiro, B., 1991. Kuwait dolocrete: petrology, geochemistry and groundwater origin. Sedimentary Geology, 73: 59-75.
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- Häusler, H., Plašienka, D. & Polák, M., 1993. Comparison of Mesozoic successions of the Central Eastern Alps and the Central Western Carpathians. Jahrbuch der Geologischen Bundesanstalt, 136: 715-739.
- Kotański, Z., 1973. Upper and middle Subtatric Nappes in the Tatra Mts. Bulletin de l'Académie Polonaisé des Science, Série des Sciences de la Terre, 21: 75-83.
- Kotański, Z., 1974. Upper and middle subtatric nappes in the Tatra Mts (In Polish, English summary). Przegląd Geologiczny, 1: 13-14.
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- Kotański, Z., 1979b. On the Triassic ofthe Tatra Mts. (In Polish, English summary). Przegląd Geologiczny, 26: 369-377.
- Kotański, Z., 1985a. Once more about the Stražov Nappe in the Tatra Mts; part I. (In Polish, English summary). Przegląd Geologiczny, 33: 547-553.
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- Limanowski, M., 1903. Perm i Tryas lądowy w Tatrach. (In Polish). Pamiętnik Towarzystwa Tatrzańskiego, 24: 140-176.
- Mc Bride, E. F., 1974. Significance of color in red, green, purple, olive, brown, and grey beds of Difunta Group, northeastern Mexico. Journal of Sedimentary Petrology, 44: 760-773.
- Michalík, J., 1993. Mesozoic tensional basin in the Alpine-Carpathian shelf. Acta Geologica Hungarica, 36: 395-403.
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- Michalík, J., 1997. Tsunamites in a stormdominated Anisian carbonate ramp (Vysoka Formation, Male Karpaty Mts, Western Carpathians). Geologica Carpathica, 48: 221-229.
- Michalík, J. & Jendrejáková, O., 1978. Organism communities and biofacies of the Fatra Formation (Uppermost Triassic, Fatric) in the Western Carpathians. Geologický Sbornik Geologica Carpathica, 29: 113-137
- Michalík, J., Masaryk, P., Lintnerowa, O., Papšová, J., Jendre-jakowa, O. & Rechakowa, D., 1992. Sedimentology and facies of storm-dominated Middle Triassic carbonate ramp (Vysoka Formation, Male Karpaty Mts, Western Carpathians). Geologica Carpathica, 43: 213-230.
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- Murray, R. C., 1990. Diagenetic silica stratification in a paleosilcrete, North Texas. Journal of Sedimentary Petrology, 60: 717-720.
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- Rychliński, T. & Szulc, J., 2005. Facies and sedimentary environments of the Upper Scythian-Carnian succession from the Belanské Tatra Mts, Slovakia. Annales Societatis Geoloogrum Poloniae, 75: 155-169.
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- Wanas, H. A. & Abu El-Hassan, M. M., 2006. Paleosols of the Upper Cretaceous-Lower Tertiary Maghra El-Bahari Formation in the northeastern portion of the Eastern Desert, Egypt: Their recognition and geological significance. Sedimentary Geology, 183:243-259.
- Warren, J. K., 1983. Pedogenic calcrete as it occurs in Quaternary calcareous dunes in costal South Australia. Journal of Sedimentary Petrology, 53: 787-796.
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Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS7-0001-0037