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Novák, M. & Škoda, R. (2007): Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences, 52(1-2), 161-167.

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Year2007
Original EntryNovák, M. & Škoda, R. (2007): Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences, 52(1-2), 161-167.
Mindat Ref. ID16005291Long-form Identifiermindat:1:5:16005291:2
GUID582a6eae-5a23-4ce3-92fb-7b221757c9aa
Full ReferenceNovák, M. & Škoda, R. (2007): Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences, 52(1-2), 161-167.
Plain TextNovák, M. & Škoda, R. (2007): Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences, 52(1-2), 161-167.

Map of Localities

Mineral Occurrences

LocalityMineral(s)
Kojetice metamanganolite occurrence, Kojetice, Třebíč District, Vysočina Region, Czech Republicⓘ Albite, ⓘ Andalusite, ⓘ Braunite, ⓘ Chernovite-(Y), ⓘ Cobaltite, ⓘ Hyalophane, ⓘ K Feldspar, ⓘ Kanonaite, ⓘ Magnetite, ⓘ Monazite-(Ce), ⓘ Muscovite, ⓘ Paragonite, ⓘ Pseudobrookite, ⓘ Pyrophanite, ⓘ Quartz, ⓘ Rutile, ⓘ Spessartine, ⓘ Tephroite

See Also

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

Novák, M., Škoda, R. (2007) Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences, 52(1-2), 161-167.
Novák, M., Škoda, R. (2007) Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of Geosciences: 52(1-2): 161-167.
Novák, M., Škoda, R. (2007) Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic. Journal of GEOsciences, 52 (1-2) 161-167
Čopjaková, R., Škoda, R., Vašinová Galiová, M., Novák, M. (2013) Distributions of Y + REE and Sc in tourmaline and their implications for the melt evolution; examples from NYF pegmatites of the Třebíč Pluton, Moldanubian Zone, Czech Republic. Journal of GEOsciences, 58 (2) 113-131
Škoda, R., Novák, M. (2012) Granitic Pegmatites of the Třebíč Syenite Pluton, Moldanubian Zone, Czech Republic; an Example of NYF to Mixed Pegmatites Related to the Orogenic Pluton. Mineralogica-Petrographica Abstract Series, Szeged: 7: 94, 120.
Novák, M., Toman, J., Škoda, R., Šikola, D., Mazuch, J. (2023) Review of zeolite mineralizations from the high-grade metamorphosed Strážek Unit, Moldanubian Zone, Czech Republic. Journal of GEOsciences, 68 (2) 111-138
Zachař, A., Novák, M., Škoda, R. (2020) Beryllium minerals as monitors of geochemical evolution from magmatic to hydrothermal stage; examples from NYF pegmatites of the Třebíč Pluton, Czech Republic. Journal of GEOsciences, 65 (3) 153-172
Škoda, R., Novák, M. (2007) Y,REE,Nb,Ta,Ti-oxide (AB2O6) minerals from REL-REE euxenite-subtype pegmatites of the Třebíč Pluton, Czech Republic; substitutions and fractionation trends. Lithos: 95: 43-57.
Novák, M., Johan, Z., Škoda, R., Černý, P., Šrein, V., & Veselovský, F. (2008). Primary oxide minerals in the system WO3–Nb2O5–TiO2–Fe2O3–FeO and their breakdown products from the pegmatite No. 3 at Dolní Bory-Hatě, Czech Republic. European Journal of Mineralogy, 20(4), 487-499.
Novák, M., Johan, Z., Škoda, R., Černý, P., Šrein, V., Veselovský, F. (2008) Primary oxide minerals in the system WO3–Nb2O5–TiO2–Fe2O3–FeO and their breakdown products from the pegmatite No. 3 at Dolní Bory-Hatě, Czech Republic. European Journal of Mineralogy, 20(4), 487-499.
Novak, M., Kadlec, T., & Gadas, P. (2013). Geological position, mineral assemblages and contamination of granitic pegmatites in the Moldanubian Zone, Czech Republic; examples from the Vlastejovice region. Journal of Geosciences, 58(1), 21-47.
 
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