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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F09%3A10001052%21RIV10-MSM-11310___
rdf:type
n6:Vysledek skos:Concept
dcterms:description
Variscan, mantle-derived peridotites and associated pyroxenites occur as boudins in Moldanubian granulite near the town of Horní Bory in western Moravia. The peridotites consist of two compositionally distinct suites, one of Mg-lherzolite (Mg-number = 89-91, 87Sr/86Sr = 0.7046-0.7068, eNd = +4.1 to +5.3), and another of Fe-dunite/wehrlite (Mg-number = 83-88, 87Sr/86Sr = 0.7079-0.7087, eNd = ?2.8 to ?1.3). Modelling of Mg-Fe exchange between peridotite and Fe-rich melts reveals that the modal and chemical composition of the Fe-dunite/wehrlite suite can be produced by melt-rock reactions between lherzolite and SiO2-undersaturated melts of basaltic composition at melt/rock ratios ranging from 0.3 to 2. In such a model, pyroxenites represent the crystalline product (+-trapped liquid) of melts migrating along conduits in peridotite. The Fe-dunite/wehrlite suite and pyroxenites are enriched in the LILE and depleted in the HFSE. The trace element and Sr-Nd isotopic compositions of Horní Bory. Variscan, mantle-derived peridotites and associated pyroxenites occur as boudins in Moldanubian granulite near the town of Horní Bory in western Moravia. The peridotites consist of two compositionally distinct suites, one of Mg-lherzolite (Mg-number = 89-91, 87Sr/86Sr = 0.7046-0.7068, eNd = +4.1 to +5.3), and another of Fe-dunite/wehrlite (Mg-number = 83-88, 87Sr/86Sr = 0.7079-0.7087, eNd = ?2.8 to ?1.3). Modelling of Mg-Fe exchange between peridotite and Fe-rich melts reveals that the modal and chemical composition of the Fe-dunite/wehrlite suite can be produced by melt-rock reactions between lherzolite and SiO2-undersaturated melts of basaltic composition at melt/rock ratios ranging from 0.3 to 2. In such a model, pyroxenites represent the crystalline product (+-trapped liquid) of melts migrating along conduits in peridotite. The Fe-dunite/wehrlite suite and pyroxenites are enriched in the LILE and depleted in the HFSE. The trace element and Sr-Nd isotopic compositions of Horní Bory.
dcterms:title
Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions
skos:prefLabel
Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt-rock reactions
skos:notation
RIV/00216208:11310/09:10001052!RIV10-MSM-11310___
n3:aktivita
n15:P n15:Z
n3:aktivity
P(IAA3013403), Z(AV0Z30130516), Z(MSM0021620855)
n3:cisloPeriodika
3-4
n3:dodaniDat
n4:2010
n3:domaciTvurceVysledku
n8:8153205 n8:8897247 n8:6847048
n3:druhVysledku
n12:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n11:predkladatel
n3:idSjednocenehoVysledku
316257
n3:idVysledku
RIV/00216208:11310/09:10001052
n3:jazykVysledku
n10:eng
n3:klicovaSlova
Geochemistry; Fe-rich peridotites; dunite- wehrlite; melt-rockreactions
n3:klicoveSlovo
n5:dunite-%20wehrlite n5:melt-rockreactions n5:Fe-rich%20peridotites n5:Geochemistry
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[9246BC7B6CD2]
n3:nazevZdroje
Chemical Geology
n3:obor
n17:DD
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
6
n3:projekt
n13:IAA3013403
n3:rokUplatneniVysledku
n4:2009
n3:svazekPeriodika
259
n3:tvurceVysledku
Siebel, Wolfgang Medaris Jr., Gordon Jelínek, Emil Ackerman, Lukáš Ježek, Josef Strnad, Ladislav
n3:wos
000264060000006
n3:zamer
n14:AV0Z30130516 n14:MSM0021620855
s:issn
0009-2541
s:numberOfPages
16
n19:organizacniJednotka
11310