About: Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic

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About: Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Layered, garnet bearing aplite pegmatite dykes of the Hlína granitic suite, ~2 to 50 m thick and up to ~200 m long with general NW SE orientation and dip 40 80 to NE or SW, cut granodiorites to granites at the SW part of the Brno Batholith, Brunovistulicum, Czech Republic. Aplite pegmatite bodies are characterized by alternation of two main textural units: (i) fine grained aplite unit with garnet stripes and (ii) coarse grained pegmatite unit with oriented Qtz, Plg and Kfs comb like crystals known as Unidirectional Solidification Textures (UST). Both units developed in zones with the thickness varying from several cm to ~1 2 m for aplite unit, and ~10 cm for the UST unit. All rock types are characterized by high contents of SiO2 (74.6 75.7 wt. %), K2O (4.61 4.94 wt. %), Na2O (3.82 4.21 wt. %), moderate concentration of CaO (0.94 1.11 wt. %), and low to very low concentrations of Fe2O3 T (0.62 0.93 wt. %), MgO (0.0 0.03 wt. %), and TiO2 ( 0.03 wt. %). Layered, garnet bearing aplite pegmatite dykes of the Hlína granitic suite, ~2 to 50 m thick and up to ~200 m long with general NW SE orientation and dip 40 80 to NE or SW, cut granodiorites to granites at the SW part of the Brno Batholith, Brunovistulicum, Czech Republic. Aplite pegmatite bodies are characterized by alternation of two main textural units: (i) fine grained aplite unit with garnet stripes and (ii) coarse grained pegmatite unit with oriented Qtz, Plg and Kfs comb like crystals known as Unidirectional Solidification Textures (UST). Both units developed in zones with the thickness varying from several cm to ~1 2 m for aplite unit, and ~10 cm for the UST unit. All rock types are characterized by high contents of SiO2 (74.6 75.7 wt. %), K2O (4.61 4.94 wt. %), Na2O (3.82 4.21 wt. %), moderate concentration of CaO (0.94 1.11 wt. %), and low to very low concentrations of Fe2O3 T (0.62 0.93 wt. %), MgO (0.0 0.03 wt. %), and TiO2 ( 0.03 wt. %). (en)
Title	Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic (en)
skos:prefLabel	Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic (en)
skos:notation	RIV/00216224:14310/10:00040659!RIV11-AV0-14310___
http://linked.open...avai/riv/aktivita	P
http://linked.open...avai/riv/aktivity	P(IAA300130801)
http://linked.open...iv/cisloPeriodika	55
http://linked.open...vai/riv/dodaniDat	2011
http://linked.open...aciTvurceVysledku	Hönig, Sven Novák, Milan Leichmann, Jaromír
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Masarykova univerzita / Přírodovědecká fakulta
http://linked.open...dnocenehoVysledku	294323
http://linked.open...ai/riv/idVysledku	RIV/00216224:14310/10:00040659
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Unidirectional Solidification Texture; magmatic layering; garnet; yttrium; aplite pegmatite; Brno Batholith (en)
http://linked.open.../riv/klicoveSlovo	garnet yttrium Unidirectional Solidification Texture aplite pegmatite Brno Batholith magmatic layering
http://linked.open...odStatuVydavatele	CZ - Česká republika
http://linked.open...ontrolniKodProRIV	[F2A9FD8FDF32]
http://linked.open...i/riv/nazevZdroje	Journal of Geosciences
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	3 (xsd:int)
http://linked.open...cetTvurcuVysledku	3 (xsd:int)
http://linked.open...vavai/riv/projekt	Chemical evolution of contrasting types of highly fractionated granitic melts using melt inclusions study
http://linked.open...UplatneniVysledku	2010
http://linked.open...v/svazekPeriodika	2010
http://linked.open...iv/tvurceVysledku	Leichmann, Jaromír Novák, Milan Hönig, Sven
issn	1802-6222
number of pages	16 (xsd:int)
http://localhost/t...ganizacniJednotka	14310
is http://linked.open...avai/riv/vysledek of	Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic Unidirectional solidification textures and garnet layering inY enriched garnet bearing aplite pegmatites in the CadomianBrno Batholith, Czech Republic

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