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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F07%3A00023827%21RIV10-MSM-14310___
rdf:type
skos:Concept n16:Vysledek
dcterms:description
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). 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).
dcterms: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 Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic
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 Mn3+-rich andalusite to kanonaite and their breakdown products from metamanganolite at Kojetice near Třebíč, the Moldanubian Zone, Czech Republic
skos:notation
RIV/00216224:14310/07:00023827!RIV10-MSM-14310___
n3:aktivita
n9:Z
n3:aktivity
Z(MSM0021622412)
n3:cisloPeriodika
1
n3:dodaniDat
n18:2010
n3:domaciTvurceVysledku
n4:4800974 n4:5413761
n3:druhVysledku
n5:J
n3:duvernostUdaju
n12:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
434133
n3:idVysledku
RIV/00216224:14310/07:00023827
n3:jazykVysledku
n17:cze
n3:klicovaSlova
Mn3+-rich andalusite; kanonaite; spessartine; paragonite; muscovite; Kojetice
n3:klicoveSlovo
n6:kanonaite n6:muscovite n6:paragonite n6:Kojetice n6:Mn3%2B-rich%20andalusite n6:spessartine
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[BD52508B79D9]
n3:nazevZdroje
Journal of Geosciences
n3:obor
n7:DB
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
2
n3:rokUplatneniVysledku
n18:2007
n3:svazekPeriodika
52
n3:tvurceVysledku
Škoda, Radek Novák, Milan
n3:zamer
n15:MSM0021622412
s:issn
1802-6222
s:numberOfPages
7
n13:organizacniJednotka
14310