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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F12%3A00383498%21RIV13-AV0-67985831
rdf:type
skos:Concept n14:Vysledek
dcterms:description
Vertical changes in chemical composition of zircon vere studied on examples of the strongly peraluminous S-type Beauvoir granite (Massif Central, France, 800 m long borehole GPF-1) and the slightly peraluminous A-type Cínovec granite (Krušné hory Mts./Erzgebirge, Czech Republic/Germany, 1596 m long borehole CS-1). At Beauvoir, zircon shows increase in Hf-content from 2-4 wt% HfO2 in the deepest B3-unit to 15-19 wt% HfO2 in the uppermost B1-unit. The highest contents of F, P, and U were detected in the intermediate unit B2 at a depth of 400-600 m. At Cínovec, Hf shows only moderate enrichment from ca 2 wt% HfO2 in the deeper protolithionite granite to 5-10 wt% HfO2 in the uppermost part of the zinnwaldite granite. Extreme enrichment of outer zones of zircon crystals with Hf or high contents of Th, U, REE, Y and Nb are not considered to be a specific phenomenon characterizing melts of A- or S-type granite, but reflects a high degree of fractionation of systems rich in Na and F. Vertical changes in chemical composition of zircon vere studied on examples of the strongly peraluminous S-type Beauvoir granite (Massif Central, France, 800 m long borehole GPF-1) and the slightly peraluminous A-type Cínovec granite (Krušné hory Mts./Erzgebirge, Czech Republic/Germany, 1596 m long borehole CS-1). At Beauvoir, zircon shows increase in Hf-content from 2-4 wt% HfO2 in the deepest B3-unit to 15-19 wt% HfO2 in the uppermost B1-unit. The highest contents of F, P, and U were detected in the intermediate unit B2 at a depth of 400-600 m. At Cínovec, Hf shows only moderate enrichment from ca 2 wt% HfO2 in the deeper protolithionite granite to 5-10 wt% HfO2 in the uppermost part of the zinnwaldite granite. Extreme enrichment of outer zones of zircon crystals with Hf or high contents of Th, U, REE, Y and Nb are not considered to be a specific phenomenon characterizing melts of A- or S-type granite, but reflects a high degree of fractionation of systems rich in Na and F.
dcterms:title
Vertical zonality of fractionated granite plutons reflected in zircon chemistry: the Cinovec A-type versus the Beauvoir S-type suite Vertical zonality of fractionated granite plutons reflected in zircon chemistry: the Cinovec A-type versus the Beauvoir S-type suite
skos:prefLabel
Vertical zonality of fractionated granite plutons reflected in zircon chemistry: the Cinovec A-type versus the Beauvoir S-type suite Vertical zonality of fractionated granite plutons reflected in zircon chemistry: the Cinovec A-type versus the Beauvoir S-type suite
skos:notation
RIV/67985831:_____/12:00383498!RIV13-AV0-67985831
n14:predkladatel
n15:ico%3A67985831
n3:aktivita
n4:S n4:P n4:I
n3:aktivity
I, P(GAP210/10/1105), P(GAP210/10/1309), S
n3:cisloPeriodika
5
n3:dodaniDat
n7:2013
n3:domaciTvurceVysledku
n18:2882442
n3:druhVysledku
n11:J
n3:duvernostUdaju
n13:S
n3:entitaPredkladatele
n9:predkladatel
n3:idSjednocenehoVysledku
177347
n3:idVysledku
RIV/67985831:_____/12:00383498
n3:jazykVysledku
n17:eng
n3:klicovaSlova
zircon; Cinovec; Beauvoir; trace elements analyses; S-type granite; A-type granite; fractionation
n3:klicoveSlovo
n5:fractionation n5:S-type%20granite n5:Cinovec n5:A-type%20granite n5:trace%20elements%20analyses n5:Beauvoir n5:zircon
n3:kodStatuVydavatele
SK - Slovenská republika
n3:kontrolniKodProRIV
[A95638482F10]
n3:nazevZdroje
Geologica Carpathica
n3:obor
n19:DD
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
2
n3:projekt
n6:GAP210%2F10%2F1105 n6:GAP210%2F10%2F1309
n3:rokUplatneniVysledku
n7:2012
n3:svazekPeriodika
63
n3:tvurceVysledku
Škoda, R. Breiter, Karel
n3:wos
000311260600003
s:issn
1335-0552
s:numberOfPages
16
n16:doi
10.2478/v10096-012-0030-6