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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F09%3A00000282%21RIV10-MZP-00025798
rdf:type
n12:Vysledek skos:Concept
dcterms:description
Skarns in the Svratka Unit, in the neighbouring part of the Moldanubian Zone and in the Kutná Hora Complex were studied with respect to their tectonometamorphic evolution, geochemistry of the major and trace elements, stable isotope geochemistry and zircon ages. The geological positions of skarns, and their structural and metamorphic record probably reflect common tectono-metamorphic evolution with that of the surroundings rocks. The geochemical characteristics, values of the oxygen isotopes and the presence of detrital zircons with a wide range of ages exclude a metasomatic origin of the skarns and point to a sedimentary-exhalative protoliths. Skarns in the Svratka Unit, in the neighbouring part of the Moldanubian Zone and in the Kutná Hora Complex were studied with respect to their tectonometamorphic evolution, geochemistry of the major and trace elements, stable isotope geochemistry and zircon ages. The geological positions of skarns, and their structural and metamorphic record probably reflect common tectono-metamorphic evolution with that of the surroundings rocks. The geochemical characteristics, values of the oxygen isotopes and the presence of detrital zircons with a wide range of ages exclude a metasomatic origin of the skarns and point to a sedimentary-exhalative protoliths.
dcterms:title
Metamorphic history of skarns, origin of their protolith and implication for genetic interpretation; an example from three units of the Bohemian Massif Metamorphic history of skarns, origin of their protolith and implication for genetic interpretation; an example from three units of the Bohemian Massif
skos:prefLabel
Metamorphic history of skarns, origin of their protolith and implication for genetic interpretation; an example from three units of the Bohemian Massif Metamorphic history of skarns, origin of their protolith and implication for genetic interpretation; an example from three units of the Bohemian Massif
skos:notation
RIV/00025798:_____/09:00000282!RIV10-MZP-00025798
n4:aktivita
n6:Z
n4:aktivity
Z(MSM0021620855), Z(MZP0002579801)
n4:cisloPeriodika
2
n4:dodaniDat
n14:2010
n4:domaciTvurceVysledku
n5:7221223 n5:2431858 n5:2216604 n5:6989969 n5:7257910 n5:2387689
n4:druhVysledku
n16:J
n4:duvernostUdaju
n7:S
n4:entitaPredkladatele
n10:predkladatel
n4:idSjednocenehoVysledku
325627
n4:idVysledku
RIV/00025798:_____/09:00000282
n4:jazykVysledku
n17:eng
n4:klicovaSlova
skarn, Bohemian Massif, petrology, geochemistry, oxygen isotopes,detrical zircon age
n4:klicoveSlovo
n8:oxygen%20isotopes n8:petrology n8:geochemistry n8:skarn n8:Bohemian%20Massif n8:detrical%20zircon%20age
n4:kodStatuVydavatele
CZ - Česká republika
n4:kontrolniKodProRIV
[95DE8C79D89D]
n4:nazevZdroje
Journal of Geosciences
n4:obor
n13:DB
n4:pocetDomacichTvurcuVysledku
6
n4:pocetTvurcuVysledku
8
n4:rokUplatneniVysledku
n14:2009
n4:svazekPeriodika
54
n4:tvurceVysledku
Pertold, Zdeněk Pertoldová, Jaroslava Konopásek, Jiří Týcová, Patricie Verner, Kryštof Pudilová, Marta Košler, Jan Košuličová, Monika
n4:zamer
n9:MSM0021620855 n9:MZP0002579801
s:issn
1802-6222
s:numberOfPages
34