This HTML5 document contains 46 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
n19http://linked.opendata.cz/ontology/domain/vavai/riv/typAkce/
dctermshttp://purl.org/dc/terms/
n11http://purl.org/net/nknouf/ns/bibtex#
n13http://linked.opendata.cz/resource/domain/vavai/riv/tvurce/
n4http://linked.opendata.cz/resource/domain/vavai/projekt/
n8http://linked.opendata.cz/ontology/domain/vavai/
shttp://schema.org/
n9http://linked.opendata.cz/resource/domain/vavai/vysledek/RIV%2F00025798%3A_____%2F03%3A00001002%21RIV07-GA0-00025798/
skoshttp://www.w3.org/2004/02/skos/core#
n3http://linked.opendata.cz/ontology/domain/vavai/riv/
n2http://linked.opendata.cz/resource/domain/vavai/vysledek/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n12http://linked.opendata.cz/ontology/domain/vavai/riv/klicoveSlovo/
n14http://linked.opendata.cz/ontology/domain/vavai/riv/duvernostUdaju/
xsdhhttp://www.w3.org/2001/XMLSchema#
n18http://linked.opendata.cz/ontology/domain/vavai/riv/jazykVysledku/
n7http://linked.opendata.cz/ontology/domain/vavai/riv/aktivita/
n17http://linked.opendata.cz/ontology/domain/vavai/riv/druhVysledku/
n16http://linked.opendata.cz/ontology/domain/vavai/riv/obor/
n10http://reference.data.gov.uk/id/gregorian-year/

Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F03%3A00001002%21RIV07-GA0-00025798
rdf:type
n8:Vysledek skos:Concept
dcterms:description
The felsic granulites with the Variscan (~340 Ma) HP?HT assemblage Grt+Qtz+hypersolvus Fsp+-Ky, correspond geochemically to slightly peraluminous, fractionated granitic rocks. U, Th and Cs are strongly depleted, probably because of the fluid and/or slight melt loss during the HP metamorphism (900?1050 C, 1?5?2?0 GPa). However, the rest of the trace-element contents and variation trends can be explained by fractional crystallisation of a granitic magma. Low Zr and LREE contents yield ~750 C Zrc and Mnz saturation temperatures and suggest relatively low-T crystallisation. The granulites contain radiogenic Sr (Sri=0?7106?0?7706) and unradiogenic Nd (EpsNdi=-4?2 to -7?5), indicating derivation from an old crustal source. The bulk of felsic granulites do not appear to represent separated, syn-metamorphic Variscan HP?HT melts. Instead, they are interpreted as metamorphosed (partly anatectic) equivalents of older, probably high-level granites subducted to continental roots during the Variscan collision. Variské felzické granulity Gföhlské jednotky moldanubika geochemicky odpovídají mírně peraluminickým, frakcionovaným granitům. Kromě silného ochuzení U, Th a Cs, což lze připsat na vrub ztrátě fluid při vysokotlaké metamorfóze, lze zastoupení většiny stopových prvků vysvětlit frakcionací granitového magmatu. Nízký obsah Zr a LREE ukazuje na saturační teploty zirkonu a monazitu kolem 750 C. Radiogenní Sr a neradiogenní Nd ukazuje na vznik ze starého korového zdroje. Celý komplex je interpretován jako metamorfované starší variské granity. The felsic granulites with the Variscan (~340 Ma) HP?HT assemblage Grt+Qtz+hypersolvus Fsp+-Ky, correspond geochemically to slightly peraluminous, fractionated granitic rocks. U, Th and Cs are strongly depleted, probably because of the fluid and/or slight melt loss during the HP metamorphism (900?1050 C, 1?5?2?0 GPa). However, the rest of the trace-element contents and variation trends can be explained by fractional crystallisation of a granitic magma. Low Zr and LREE contents yield ~750 C Zrc and Mnz saturation temperatures and suggest relatively low-T crystallisation. The granulites contain radiogenic Sr (Sri=0?7106?0?7706) and unradiogenic Nd (EpsNdi=-4?2 to -7?5), indicating derivation from an old crustal source. The bulk of felsic granulites do not appear to represent separated, syn-metamorphic Variscan HP?HT melts. Instead, they are interpreted as metamorphosed (partly anatectic) equivalents of older, probably high-level granites subducted to continental roots during the Variscan collision.
dcterms:title
Whole-rock geochemistry and genesis of the granulites from the Gföhl Unit (Moldanubian Zone of the Bohemian Massif, Austria and Czech Republic) Whole-rock geochemistry and genesis of the granulites from the Gföhl Unit (Moldanubian Zone of the Bohemian Massif, Austria and Czech Republic) Horninová geochemie a geneze granulitů Gföhlské jednotky (Moldanubikum Českého masivu, Rakousko a Česká republika)
skos:prefLabel
Whole-rock geochemistry and genesis of the granulites from the Gföhl Unit (Moldanubian Zone of the Bohemian Massif, Austria and Czech Republic) Horninová geochemie a geneze granulitů Gföhlské jednotky (Moldanubikum Českého masivu, Rakousko a Česká republika) Whole-rock geochemistry and genesis of the granulites from the Gföhl Unit (Moldanubian Zone of the Bohemian Massif, Austria and Czech Republic)
skos:notation
RIV/00025798:_____/03:00001002!RIV07-GA0-00025798
n3:strany
57-57
n3:aktivita
n7:P
n3:aktivity
P(GA205/03/0040)
n3:dodaniDat
n10:2007
n3:domaciTvurceVysledku
n13:7243111
n3:druhVysledku
n17:D
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n9:predkladatel
n3:idSjednocenehoVysledku
635526
n3:idVysledku
RIV/00025798:_____/03:00001002
n3:jazykVysledku
n18:eng
n3:klicovaSlova
Austria, Czech Republic, high-grade metamorphism, Nd isotopes, partial melting, Sr isotopes, Variscan orogeny
n3:klicoveSlovo
n12:high-grade%20metamorphism n12:Variscan%20orogeny n12:Czech%20Republic n12:Austria n12:Sr%20isotopes n12:partial%20melting n12:Nd%20isotopes
n3:kontrolniKodProRIV
[28153CF51FA1]
n3:mistoKonaniAkce
Toyohashi
n3:mistoVydani
Tsukuba
n3:nazevZdroje
Hutton Symposium V : the Origin of Granites and Related Rocks Japan 2003 : abstract with program
n3:obor
n16:DD
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
2
n3:projekt
n4:GA205%2F03%2F0040
n3:rokUplatneniVysledku
n10:2003
n3:tvurceVysledku
Janoušek, Vojtěch Finger, Fritz
n3:typAkce
n19:WRD
n3:zahajeniAkce
2003-01-01+01:00
s:numberOfPages
1
n11:hasPublisher
Geological Survey of Japan