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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F11%3A00367548%21RIV12-AV0-67985831
rdf:type
n8:Vysledek skos:Concept
dcterms:description
The lattice-preferred orientation (LPOs) of two late-Variscan granitoids, the Meissen monzonite and the Podlesí dyke granite, were determined from high-resolution time-of-flight neutron diffraction patterns gained at the diffractometer SKAT in Dubna, Russia. The results demonstrate that the method is suitable for the LPO analysis of polyphase, relatively coarse-grained (0.1–6 mm) rocks. The Meissen monzonite has a prominent shape-preferred orientation (SPO) of the non-equidimensional minerals feldspar, mica and amphibole, whereas SPO of the Podlesí granite is unapparent at the hand-specimen scale. The neutron diffraction data revealed distinct LPOs in both granitoids. The LPO of the non-equidimensional minerals feldspar, mica and amphibole developed mainly during magmatic flow. The lattice-preferred orientation (LPOs) of two late-Variscan granitoids, the Meissen monzonite and the Podlesí dyke granite, were determined from high-resolution time-of-flight neutron diffraction patterns gained at the diffractometer SKAT in Dubna, Russia. The results demonstrate that the method is suitable for the LPO analysis of polyphase, relatively coarse-grained (0.1–6 mm) rocks. The Meissen monzonite has a prominent shape-preferred orientation (SPO) of the non-equidimensional minerals feldspar, mica and amphibole, whereas SPO of the Podlesí granite is unapparent at the hand-specimen scale. The neutron diffraction data revealed distinct LPOs in both granitoids. The LPO of the non-equidimensional minerals feldspar, mica and amphibole developed mainly during magmatic flow.
dcterms:title
Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms
skos:prefLabel
Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms
skos:notation
RIV/67985831:_____/11:00367548!RIV12-AV0-67985831
n8:predkladatel
n9:ico%3A67985831
n3:aktivita
n13:Z
n3:aktivity
Z(AV0Z30130516)
n3:cisloPeriodika
7
n3:dodaniDat
n10:2012
n3:domaciTvurceVysledku
n18:2882442
n3:druhVysledku
n15:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n12:predkladatel
n3:idSjednocenehoVysledku
209055
n3:idVysledku
RIV/67985831:_____/11:00367548
n3:jazykVysledku
n5:eng
n3:klicovaSlova
neutron diffraction; lattice-preferred orientation; shape-preferred orientation; magmatic flow; Podlesí granite; Meissen massif
n3:klicoveSlovo
n7:Meissen%20massif n7:Podles%C3%AD%20granite n7:neutron%20diffraction n7:magmatic%20flow n7:shape-preferred%20orientation n7:lattice-preferred%20orientation
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[1663DD8DBC17]
n3:nazevZdroje
International Journal of Earth Sciences
n3:obor
n19:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
4
n3:rokUplatneniVysledku
n10:2011
n3:svazekPeriodika
100
n3:tvurceVysledku
Ullemeyer, K. Müller, A. Leiss, B. Breiter, Karel
n3:wos
000295534200005
n3:zamer
n4:AV0Z30130516
s:issn
1437-3254
s:numberOfPages
18
n17:doi
10.1007/s00531-010-0590-6