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Statements

Subject Item
n2:RIV%2F61989592%3A15310%2F12%3A33141928%21RIV13-MSM-15310___
rdf:type
skos:Concept n16:Vysledek
dcterms:description
Common pegmatites with pockets lined with crystals of smoky quartz, feldspars, muscovite, and black tourmaline commonly occur in migmatized biotite-sillimanite gneisses and felsic granulites of the Strážek Unit, Moldanubian Zone, in the Czech Republic. Mostly concordant dikes or irregular bodies (0.1-2 m thick) consisting of an outer granitic unit, a graphic unit and a pocket unit with large crystals (up to 1 m long) of minerals show transitional to locally sharp contacts to the host migmatized rocks. Thin muscovite-rich veins, 1-10 cm thick, with the assemblage muscovite ? albite, quartz and tourmaline are closely associated spatially. Variable prismatic to lens-shaped tourmaline crystals and their aggregates, up to 30 cm across, from pockets and muscovite-rich veins exhibit striking zoning in the optical microscope (distinct colors and pleochroism) and in BSE images: core (foitite - schorl - magnesio-foitite), intermediate zone (schorl - dravite) and narrow outer rim (schorl - dravite); tourmaline from muscovite veins is relatively homogeneous (dravite - magnesio-foitite). A slight decrease in X-site vacancy, in Fetot/(Fetot + Mg) and Al contents but sharp increase of Ti from the core to intermediate zone and outer rim, respectively, are typical. Also, the LA-ICP-MS study of a single crystal of tourmaline from a pocket demonstrates a very similar chemical composition of core and intermediate zone, but a distinct composition of outer rim; Mn, Ni, Zn, Sc and Ga decrease, and V, Cr, Co and Sr increase in the rim. Nearly all Fe was determined as Fe2+ ({3% of Fe3+ in both core and intermediate zones of the tourmaline) using Mössbauer spectroscopy. Common pegmatites with pockets lined with crystals of smoky quartz, feldspars, muscovite, and black tourmaline commonly occur in migmatized biotite-sillimanite gneisses and felsic granulites of the Strážek Unit, Moldanubian Zone, in the Czech Republic. Mostly concordant dikes or irregular bodies (0.1-2 m thick) consisting of an outer granitic unit, a graphic unit and a pocket unit with large crystals (up to 1 m long) of minerals show transitional to locally sharp contacts to the host migmatized rocks. Thin muscovite-rich veins, 1-10 cm thick, with the assemblage muscovite ? albite, quartz and tourmaline are closely associated spatially. Variable prismatic to lens-shaped tourmaline crystals and their aggregates, up to 30 cm across, from pockets and muscovite-rich veins exhibit striking zoning in the optical microscope (distinct colors and pleochroism) and in BSE images: core (foitite - schorl - magnesio-foitite), intermediate zone (schorl - dravite) and narrow outer rim (schorl - dravite); tourmaline from muscovite veins is relatively homogeneous (dravite - magnesio-foitite). A slight decrease in X-site vacancy, in Fetot/(Fetot + Mg) and Al contents but sharp increase of Ti from the core to intermediate zone and outer rim, respectively, are typical. Also, the LA-ICP-MS study of a single crystal of tourmaline from a pocket demonstrates a very similar chemical composition of core and intermediate zone, but a distinct composition of outer rim; Mn, Ni, Zn, Sc and Ga decrease, and V, Cr, Co and Sr increase in the rim. Nearly all Fe was determined as Fe2+ ({3% of Fe3+ in both core and intermediate zones of the tourmaline) using Mössbauer spectroscopy.
dcterms:title
Compositional evolution of zoned tourmaline crystals from pockets in common pegmatites of the Moldanubian zone, Czech Republic Compositional evolution of zoned tourmaline crystals from pockets in common pegmatites of the Moldanubian zone, Czech Republic
skos:prefLabel
Compositional evolution of zoned tourmaline crystals from pockets in common pegmatites of the Moldanubian zone, Czech Republic Compositional evolution of zoned tourmaline crystals from pockets in common pegmatites of the Moldanubian zone, Czech Republic
skos:notation
RIV/61989592:15310/12:33141928!RIV13-MSM-15310___
n16:predkladatel
n17:orjk%3A15310
n3:aktivita
n15:Z n15:P
n3:aktivity
P(ED2.1.00/03.0058), P(GAP210/10/0743), Z(MSM0021622412)
n3:cisloPeriodika
4
n3:dodaniDat
n9:2013
n3:domaciTvurceVysledku
n18:5207193
n3:druhVysledku
n20:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n5:predkladatel
n3:idSjednocenehoVysledku
128238
n3:idVysledku
RIV/61989592:15310/12:33141928
n3:jazykVysledku
n19:eng
n3:klicovaSlova
foitite, schorl, dravite, magnesio-foitite, compositional evolution, zoning, pocket, common pegmatite, Moldanubian Zone, Czech Republic
n3:klicoveSlovo
n4:compositional%20evolution n4:foitite n4:zoning n4:schorl n4:Moldanubian%20Zone n4:common%20pegmatite n4:pocket n4:dravite n4:Czech%20Republic n4:magnesio-foitite
n3:kodStatuVydavatele
CA - Kanada
n3:kontrolniKodProRIV
[F8CA33EEBCFC]
n3:nazevZdroje
Canadian Mineralogist
n3:obor
n21:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
5
n3:projekt
n6:ED2.1.00%2F03.0058 n6:GAP210%2F10%2F0743
n3:rokUplatneniVysledku
n9:2012
n3:svazekPeriodika
50
n3:tvurceVysledku
Gadas, Petr Vašinová - Galiová, Michaela Staněk, Josef Filip, Jan Novák, Milan
n3:wos
000314174400010
n3:zamer
n13:MSM0021622412
s:issn
0008-4476
s:numberOfPages
18
n14:doi
10.3749/canmin.50.4.895
n11:organizacniJednotka
15310