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Ackerman, L. (2005). Magmatic vs. hydrothermal origin of fluorites from Vlastejovice, Bohemian Massif. Journal of GEOsciences, 50(1/2), 35.

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Reference Type- plain text -
Year2005
Original EntryAckerman, L. (2005). Magmatic vs. hydrothermal origin of fluorites from Vlastejovice, Bohemian Massif. Journal of GEOsciences, 50(1/2), 35.
Mindat Ref. ID15941708Long-form Identifiermindat:1:5:15941708:1
GUID0
Full ReferenceAckerman, L. (2005). Magmatic vs. hydrothermal origin of fluorites from Vlastejovice, Bohemian Massif. Journal of GEOsciences, 50(1/2), 35.
Plain TextAckerman, L. (2005). Magmatic vs. hydrothermal origin of fluorites from Vlastejovice, Bohemian Massif. Journal of GEOsciences, 50(1/2), 35.

Mineral Occurrences

LocalityMineral(s)
Vlastějovice, Kutná Hora District, Central Bohemian Region, Czech Republicⓘ Almandine, ⓘ Amphibolite, ⓘ Anatase, ⓘ Andradite, ⓘ Bavenite, ⓘ Biotite, ⓘ Calcite, ⓘ Columbite-(Mn), ⓘ Datolite, ⓘ Eclogite, ⓘ Elbaite, ⓘ Epidote, ⓘ Fluorite, ⓘ Garnet Group, ⓘ Gneiss, ⓘ Grossular, Hornblende, ⓘ Magnetite, ⓘ Oligoclase, ⓘ Pegmatite, ⓘ Pyrochlore Group, ⓘ Quartz, ⓘ Quartzite, ⓘ Schorl, ⓘ Skarn, ⓘ Thorite, ⓘ Titanite, ⓘ Uraninite

See Also

These are possibly similar items as determined by title/reference text matching only.

Ackerman, L. (2005) Magmatic vs. hydrothermal origin of fluorites from Vlastějovice, Bohemian Massif. Journal of the Czech Geological Society, 50 (1-2) 35-41
ACKERMAN, L. (2005): Magmatic vs. hydrotermal origin of fluorites from Vlastějovice, Bohemian Massif. - Journal of the Czech Geological Society, 50/1-2, Praha.
Zachariáš, J. (2008) Compositional trends in magmatic and hydrothermal silicates of the Petráčkova hora intrusive complex, Bohemian Massif - link between the magmatic processes and intrusion-related gold mineralization. Journal of GEOsciences, 53 (1) 105-117
Veselovský, F., Pašava, J., Pour, O., Ackerman, L. (2021) Origin of V-Cr-Ti-mineralization in thermally overprinted metal-rich black shales from the Teplá-Barrandian Unit (Bohemian Massif) and implications for metal remobilization during metamorphism. Journal of GEOsciences, 66 (4) 263-275
Trubač, J., Vrána, S., Haluzová, E., Ackerman, L. (2015) Petrology and geochemical characteristics of phlogopite pyroxenite related to durbachites, Moldanubian Zone, Bohemian Massif. Journal of GEOsciences, 60 (2) 73-90
Ackerman, L., Špaček, P., Medaris Jr, G., Hegner, E., Svojtka, M., Ulrych, J. (2012) Geochemistry and petrology of pyroxenite xenoliths from Cenozoic alkaline basalts, Bohemian Massif. Journal of GEOsciences, 57 (4) 199-219
Ackerman, L., Spacek, P., Medaris Jr, G., Hegner, E., Svojtka, M., & Ulrych, J. (2012). Geochemistry and petrology of pyroxenite xenoliths from Cenozoic alkaline basalts, Bohemian Massif. Journal of Geosciences, 57(4), 199-219.
Žák, K., Ackerman, L., Veselovský, F., Pašava, J., Dobeš, P., Svojtka, M., Creaser, R.A. (2024) Multistage hydrothermal vein mineralization in low-grade metamorphosed rocks: Chříč locality, Teplá-Barrandian Unit, Bohemian Massif, Czech Republic. Journal of Geosciences, 281-299 doi:10.3190/jgeosci.381
Buriánek, D., Hrdličková, K., Hanžl, P. (2009) Geological position and origin of augen gneisses from the Polička Unit, eastern Bohemian Massif. Journal of GEOsciences, 54 (2) 201-219
Drahota, P., Pertold, Z., Pudilová, M. (2005) Three types of skarn in the northern part of the Moldanubian zone, Bohemian Massif - Implications for their origin. Journal of the Czech Geological Society, 50 (1-2) 19-33
Knésl, I., & Ackerman, L. (2005, August). PGE mineralisation of the Bohemian Massif, Czech Republic: An overview. In 10th International Platinum Symposium ‘Platinum-Group Elements-from Genesis to Beneficiation and Environmental Impact (pp. 408-411).
 
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