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Tytuł artykułu

Megacrysts of kyanite from Baranec Mt., Western Tatra Mountains, Slovakia

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Large crystals of kyanite (<15 cm in size) occur in quartz segregations in Paleozoic gneissses on Baranec Mt., Western Tatra Mountains, northern Slovakia. Blue kyanite crystals coexist with quartz and plagioclase. The kyanite contains inclusions of apatite, monazite. gamet, rutile and biotite and overgrowths of retrograde sillimanite. muscovite and biotite. The kyanite crystals are the largest found up to now in the Tatra crystalline massif or in the other Western Carpathians crystalline cores. Kyanite. with the co-existing mineral assemblage, is indicative of a HP stage duiing Hercynian metamorphism of the Western Tatra Mountains.
Czasopismo
Rocznik
Strony
31--37
Opis fizyczny
Bibliogr. 22 poz., rys., tab., fot.
Twórcy
autor
  • Universisty of Silesia, Faculty of Earth Sciences, Będzińska st. 60, 41-200 Sosnowiec, Poland
autor
  • Universisty of Silesia, Faculty of Earth Sciences, Będzińska st. 60, 41-200 Sosnowiec, Poland
autor
  • Universisty of Silesia, Faculty of Earth Sciences, Będzińska st. 60, 41-200 Sosnowiec, Poland
Bibliografia
  • Allaz, J., Maeder, X., Vannay, J.C., & Steck, A. (2005). Formation of aluminosilicate-bearing quartz veins in the Simano nappe (Central Alps): structural, thermobarometric and oxygen constraints. Schweizerische Mineralogische und Petrographische Mitteilungen, 85, 191-214.
  • Andrusov, D. (1968). Grundriss der Tektonik der Nördlichen Karpaten. Bratislava: Verlag der Slowakischen Akademie der Wissenschaften (in German).
  • Bac-Moszaszwili, M. (1996). Podnoszenie masywu Tatr w trzecio- i czwartorzędzie. Tertiary-Quaternary uplift of the Tatra massif. In: Kotarba A. (Ed.), Przyroda Tatrzańskiego Parku Narodowego a człowiek. Tom 1. Nauki o Ziemi. TPB, PTPNoZ Oddz. Krakowie, Kraków - Zakopane, 68-71 (in Polish).
  • Běluša, J. (2000). Kyanit z Ústupu u Olešnice. Minerál, VII, 5, 424-425.
  • Faye, G. H., & Nickel, E. H. (1969). On the origin of colour and pleochroism of kyanite. Canadian Mineralogist, 10, 35-46.
  • Gawęda, A. (2009). Enclaves in the High Tatra granite. Katowice: University of Silesia Publishing House (in Polish with English abstract).
  • Gawęda, A., Kozłowski, K., & Piotrowska, K. (1998). Tectonic development of the crystalline basement of the Polish part of the Western Tatra Mts. Acta Universitatis Carolinea-Geologica, 42(2), 252-253.
  • Gawęda, A., Winchester, J. Kozłowski, K., Narębski, W., & Holland, G. (2000). Geochemistry and paleotectonic settings of the amphibolites from the Western Tatra Mountains. Geological Journal, 35, 69-85.
  • Hovorka, D. (1981). Minerály metamorfovaných hornin. Západní Karpaty. In Bernard J. H. (Ed.) Mineralogie Československa (p. 648). Praha: Academia.
  • Janák, M. (1994). Variscan uplift of the crystalline basement, Tatra Mts., Central western Carphatians: evidences from 40Ar/39Ar laser probe dating of biotite and P-T-t paths. Geologica Carphatica, 45(5), 293-300.
  • Janák, M., O`Brien, P.J., Hurai, V., & Reutel, C. (1996). Metamorphic evolution and fluid composition of garnet-clinopyroxene amphibolites from the Tatra Mountains, Western Carpathians. Lithos, 39, 57-79.
  • Janák, M., Kahan, Š., & Jančula, D. (1988). Metamorphism of pelitic rocks and metamorphic zones in SW part of Western Tatra Mts. crystalline complexes. Geologický Zborník – Geologica Carpathica, 39, 455-488.
  • Kahan, Š. (1965). Výskyt disténu v kryštaliniku Vysokých Tatier. Zprávy Geologického Výskumu vr. 1964, časť 2. Bratislava, 17-18 (in Slovak).
  • Kahan, Š. (1968). K problematike vystupovania staurolitu, disténu, sillimanitu a korundu v kryštaliniku Západných Karpát. Acta Geologica et Geographica Universitatis Comenianae, Geologica, 13, 191-202 (in Slovak).
  • Kahan, Š., & Hvožďara, P. (1967). Distén - nový minerál v kryštaliniku Vysokých Tatier. Acta Geologica et Geographica Universitatis Comenianae, Geologica, 12, 105-121 (in Slovak).
  • Kerrick, D.M. (1990). The Al2SiO5 polymorphs. In Ribbe, P.H. (ed.), Orthosilicates, Reviews in Mineralogy, 5 (pp. 189-214). Chantilly, Virginia: Mineralogical Society of America.
  • Kohut, M., & Janák, M. (1994). Granitoids of the Tatra Mts. Western Carphatians: Field relations and petrogenetic implications. Geologica Carphatica, 45(5), 301-311.
  • Mahel', M., & Buday, T. (Eds.) (1968). Regional geology of Czechoslovakia. Part II: The Western Carpathians. Praha: Academia.
  • Müller, F. (1984). Bayerns steinreiche Ecke, 2nd ed., Oberfränkische Verlagsanstalt (Hof) (in German).
  • Nabelek, P.I. (1997). Quartz-sillimanite leucosomes in the high-grade schists, Black hills, South Dacota: a perspective on the mobility of Al in high-grade metamorphic rocks. Geology, 25(11), 995-998.
  • Newton, R.C., & Manning, C.E. (2008). Solubility of corundum in the system Al2O3-SiO2-H2O-NaCl at 800o C and 10 kbar. Chemical Geology, 249(3-4), 250-261.
  • Pyka, P., Szopa, K., Gawęda, A., & Krzykawski, T. (2013). Kyanite-quartz segregations in the metamorphic complex of the Western Tatra Mountains, Central Western Carpathians. In: Broska I., & Tomašových A. (Eds.): GEEWEC 2013. Geological evolution of the Western Carpathians: new ideas in the field of inter-regional correlations. Abstract book. Bratislava: Geological Institute, Slovak Academy of Science.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-cdab34d0-d433-4ff8-b0c4-fa7be5f94851
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