| Pertoldová, J., Košuličová, M., Verner, K., Žáčková, E., Pertold, Z., Konopásek, J., Veselovský, F., Košler, J. (2014) Geochronology and petrology of pyroxene-garnet skarns (eastern Bohemian Massif): implications for the source and evolution of the Variscan continental crust. Journal of GEOsciences, 59 (4) 367-388 | Journal (article/letter/editorial) | Jan Košler1,3† 1 Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic; jaroslava.pertoldova@geology...Charles University, Albertov 6, 128 43 Prague 2, Czech Republic 3 Centre for Geobiology and Department of Earth...this age are dominant in skarns with massive magnetite mineralization, while the non-mineralized samples...pyroxene–garnet skarns grading to garnetite ± quartz and magnetite skarns). Petrological studies of skarns in the...Microanalysis of the Masaryk University and the Czech Geological Survey in Brno. Operating conditions | | | Book | (Russia), P. Bruneton (Europe), J. Cisovsky (Slovak Republic), G. Érdi-Krausz (Hungary), H. J. Förster (Germany)...Hruby (Czech Republic), E. Kirchner (Austria), B. Kirchner (Austria), J. Komínek (Czech Republic), I. Bojkov...J. Royall (Spain), and A. Kuestermeyer (Slovak Republic). M. Cuney deserves my particular gratitude for... . . . . . . . . . . . . . . . 2.1 West Balkan Region . . . . . . . . . . . . . . . . . . . . . . . .... . . . . . . . . . . . . . . . 2.1.1 Bukhovo District .. . . . . . . . . . . . . . . . . . . . . . | | Pertoldová, J., Týcová, P., Verner, K., Košuličová, M., Pertold, Z., Košler, J., Konopásek, J., Pudilová, M. (2009) Metamorphic history of skarns, origin of their protolith and implications for genetic interpretation; an example from three units of the Bohemian Massif. Journal of GEOsciences, 54 (2) 101-134 | Journal (article/letter/editorial) | Pudilová2 1 2 3 * Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic; jaroslava.pertoldova@geology...Charles University, Albertov 6, Prague 2, 128 43, Czech Republic Centre for Geobiology and Department of Earth...clinopyroxene, are accompanied by less abundant magnetite, amphibole, plagioclase, epidote ± quartz. In...amphibolite-facies conditions. The presence of magnetite and the increasing proportion of the andradite...contents vary from 8 to 345 ppm. The lowest ΣREE values (< 100 ppm) occur in skarns with magnetite mineralization |
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