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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F09%3A00000152%21RIV10-MZP-00025798
rdf:type
skos:Concept n11:Vysledek
dcterms:description
Three main Variscan tectono-metamorphic units with distinct metamorphic evolution are present at the eastern boundary of the Bohemian Massif: Moldanubian Zone (MZ), Svratka Unit (SU) and Polička Unit (PU). All these metamorphic complexes contain calc-silicate rocks, which occur as bodies, layers or nodules within gneisses, mica schists, marbles, amphibolites or skarns. Two groups of calc-silicate rocks are distinguished according to the presence/absence of garnet. The appearance of garnet is the result of continuous reactions among Fe-Ca-Al minerals. The dominant garnet-producing reaction calcite + quartz + clinozoisite = garnet + H2O + 5CO2 depends on the P–T conditions, XCO2 in the coexisting metamorphic fluids and bulk rock chemistry. Three main Variscan tectono-metamorphic units with distinct metamorphic evolution are present at the eastern boundary of the Bohemian Massif: Moldanubian Zone (MZ), Svratka Unit (SU) and Polička Unit (PU). All these metamorphic complexes contain calc-silicate rocks, which occur as bodies, layers or nodules within gneisses, mica schists, marbles, amphibolites or skarns. Two groups of calc-silicate rocks are distinguished according to the presence/absence of garnet. The appearance of garnet is the result of continuous reactions among Fe-Ca-Al minerals. The dominant garnet-producing reaction calcite + quartz + clinozoisite = garnet + H2O + 5CO2 depends on the P–T conditions, XCO2 in the coexisting metamorphic fluids and bulk rock chemistry.
dcterms:title
Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone
skos:prefLabel
Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone Garnet-forming reactions in calc-silicate rocks from the Polička Unit, Svratka Unit and SE part of the Moldanubian Zone
skos:notation
RIV/00025798:_____/09:00000152!RIV10-MZP-00025798
n4:aktivita
n13:Z
n4:aktivity
Z(MZP0002579801)
n4:cisloPeriodika
3
n4:dodaniDat
n9:2010
n4:domaciTvurceVysledku
n10:2431858 n10:6772676
n4:druhVysledku
n17:J
n4:duvernostUdaju
n15:S
n4:entitaPredkladatele
n12:predkladatel
n4:idSjednocenehoVysledku
315965
n4:idVysledku
RIV/00025798:_____/09:00000152
n4:jazykVysledku
n7:eng
n4:klicovaSlova
calc-silicate rocks, Polička Unit, Svratka Unit, Moldanubian Zone, P–T conditions, Czech Republic
n4:klicoveSlovo
n6:Svratka%20Unit n6:calc-silicate%20rocks n6:Moldanubian%20Zone n6:Czech%20Republic n6:Poli%C4%8Dka%20Unit n6:P%E2%80%93T%20conditions
n4:kodStatuVydavatele
CZ - Česká republika
n4:kontrolniKodProRIV
[4C78525D21E0]
n4:nazevZdroje
Journal of Geosciences
n4:obor
n14:DB
n4:pocetDomacichTvurcuVysledku
2
n4:pocetTvurcuVysledku
2
n4:rokUplatneniVysledku
n9:2009
n4:svazekPeriodika
54
n4:tvurceVysledku
Pertoldová, Jaroslava Buriánek, David
n4:zamer
n16:MZP0002579801
s:issn
1802-6222
s:numberOfPages
24