About: Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic     Goto   Sponge   NotDistinct   Permalink

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  • A zoned Mn3+-rich andalusite to kanonaite occurs as shortly prismatic, black-green crystals, up to 2 mm in size, randomly distributed in quartz matrix of quartzitic rock with metamanganolite portions from Kojetice near Třebíč. Minor spessartine, braunite, K-feldspar, albite, hyalophane, rare paragonite and accessory magnetite-rutile intergrowths, tephroite, chernovite-(Y), monazite-(Ce), pyrophanite, Sb-rich rutile, cobaltite, pseudobrookite(?) and pale pink flakes of late muscovite were identified in this rock. Zoned subhedral grains of Mn3+-rich andalusite to kanonaite have strong pleochroism: X = yellow, Y = green, Z = deep green, when narrow Mn3+-enriched rims feature slightly more intensive colors. Electron microprobe study shows that the core has always lower contents of Mn2O3 relative to commonly narrow rim of kanonaite. Chemical composition varies from Mn3+-rich andalusite with 0.21 apfu Mn3+ (9.72 wt. % Mn2O3) to kanonaite with up to 0.60 apfu Mn3+ (26.09 wt. % Mn2O3).
  • A zoned Mn3+-rich andalusite to kanonaite occurs as shortly prismatic, black-green crystals, up to 2 mm in size, randomly distributed in quartz matrix of quartzitic rock with metamanganolite portions from Kojetice near Třebíč. Minor spessartine, braunite, K-feldspar, albite, hyalophane, rare paragonite and accessory magnetite-rutile intergrowths, tephroite, chernovite-(Y), monazite-(Ce), pyrophanite, Sb-rich rutile, cobaltite, pseudobrookite(?) and pale pink flakes of late muscovite were identified in this rock. Zoned subhedral grains of Mn3+-rich andalusite to kanonaite have strong pleochroism: X = yellow, Y = green, Z = deep green, when narrow Mn3+-enriched rims feature slightly more intensive colors. Electron microprobe study shows that the core has always lower contents of Mn2O3 relative to commonly narrow rim of kanonaite. Chemical composition varies from Mn3+-rich andalusite with 0.21 apfu Mn3+ (9.72 wt. % Mn2O3) to kanonaite with up to 0.60 apfu Mn3+ (26.09 wt. % Mn2O3). (en)
  • A zoned Mn3+-rich andalusite to kanonaite occurs as shortly prismatic, black-green crystals, up to 2 mm in size, randomly distributed in quartz matrix of quartzitic rock with metamanganolite portions from Kojetice near Třebíč. Minor spessartine, braunite, K-feldspar, albite, hyalophane, rare paragonite and accessory magnetite-rutile intergrowths, tephroite, chernovite-(Y), monazite-(Ce), pyrophanite, Sb-rich rutile, cobaltite, pseudobrookite(?) and pale pink flakes of late muscovite were identified in this rock. Zoned subhedral grains of Mn3+-rich andalusite to kanonaite have strong pleochroism: X = yellow, Y = green, Z = deep green, when narrow Mn3+-enriched rims feature slightly more intensive colors. Electron microprobe study shows that the core has always lower contents of Mn2O3 relative to commonly narrow rim of kanonaite. Chemical composition varies from Mn3+-rich andalusite with 0.21 apfu Mn3+ (9.72 wt. % Mn2O3) to kanonaite with up to 0.60 apfu Mn3+ (26.09 wt. % Mn2O3). (cs)
Title
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic (en)
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic (cs)
skos:prefLabel
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic (en)
  • Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic (cs)
skos:notation
  • RIV/00216224:14310/07:00023827!RIV10-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM0021622412)
http://linked.open...iv/cisloPeriodika
  • 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 434133
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/07:00023827
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Mn3+-rich andalusite; kanonaite; spessartine; paragonite; muscovite; Kojetice (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [BD52508B79D9]
http://linked.open...i/riv/nazevZdroje
  • Journal of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 52
http://linked.open...iv/tvurceVysledku
  • Novák, Milan
  • Škoda, Radek
http://linked.open...n/vavai/riv/zamer
issn
  • 1802-6222
number of pages
http://localhost/t...ganizacniJednotka
  • 14310
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