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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F09%3A00330543%21RIV10-AV0-67985530
rdf:type
skos:Concept n17:Vysledek
dcterms:description
Exsolution lamellae of garnet in clinopyroxene and orthopyroxene porphyroclasts from garnet pyroxenites in the Moldanubian zone were studied to elucidate the pressure-temperature conditions of the exsolution process and to reconstruct the burial and exhumation path of ultramafic rocks in the Variscan orogen. The porphyroclasts occur in a fine-grained matrix with metamorphic fabrics, which consists of clinopyroxene and small amounts of garnet, orthopyroxene and amphibole. The clinopyroxene porphyroclasts contain garnet + orthopyroxene lamellae as well as ilmenite rods that have orientation parallel to planes of the porphyroclasts. Orthopyroxene porphyroclasts host garnet and clinopyroxene lamellae, which show the same lattice preferred orientation. In both cases, lamellar orthopyroxene, clinopyroxene and garnet were partially replaced by secondary amphibole. Exsolution lamellae of garnet in clinopyroxene and orthopyroxene porphyroclasts from garnet pyroxenites in the Moldanubian zone were studied to elucidate the pressure-temperature conditions of the exsolution process and to reconstruct the burial and exhumation path of ultramafic rocks in the Variscan orogen. The porphyroclasts occur in a fine-grained matrix with metamorphic fabrics, which consists of clinopyroxene and small amounts of garnet, orthopyroxene and amphibole. The clinopyroxene porphyroclasts contain garnet + orthopyroxene lamellae as well as ilmenite rods that have orientation parallel to planes of the porphyroclasts. Orthopyroxene porphyroclasts host garnet and clinopyroxene lamellae, which show the same lattice preferred orientation. In both cases, lamellar orthopyroxene, clinopyroxene and garnet were partially replaced by secondary amphibole.
dcterms:title
Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: constraining the early pre-convergence history of ultramafic rocks in the Variscan orogen Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: constraining the early pre-convergence history of ultramafic rocks in the Variscan orogen
skos:prefLabel
Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: constraining the early pre-convergence history of ultramafic rocks in the Variscan orogen Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: constraining the early pre-convergence history of ultramafic rocks in the Variscan orogen
skos:notation
RIV/67985530:_____/09:00330543!RIV10-AV0-67985530
n3:aktivita
n5:P n5:Z
n3:aktivity
P(GA205/06/0688), P(GP205/09/P135), Z(AV0Z30120515), Z(MSM0021620855)
n3:cisloPeriodika
9
n3:dodaniDat
n7:2010
n3:domaciTvurceVysledku
n11:5449820
n3:druhVysledku
n18:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n4:predkladatel
n3:idSjednocenehoVysledku
315964
n3:idVysledku
RIV/67985530:_____/09:00330543
n3:jazykVysledku
n16:eng
n3:klicovaSlova
Bohemian Massif; clinopyroxenite; decompression; garnet lamellae
n3:klicoveSlovo
n12:decompression n12:clinopyroxenite n12:garnet%20lamellae n12:Bohemian%20Massif
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[B5EEDE5B0A75]
n3:nazevZdroje
Journal of Metamorphic Geology
n3:obor
n14:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
3
n3:projekt
n6:GA205%2F06%2F0688 n6:GP205%2F09%2FP135
n3:rokUplatneniVysledku
n7:2009
n3:svazekPeriodika
27
n3:tvurceVysledku
Machek, Matěj Faryad, S. W. Dolejš, D.
n3:wos
000271523900005
n3:zamer
n9:AV0Z30120515 n9:MSM0021620855
s:issn
0263-4929
s:numberOfPages
17