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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F08%3A00000257%21RIV09-MZP-00025798
rdf:type
n17:Vysledek skos:Concept
dcterms:description
In the porphyritic Jizera granite, Bohemian Massif, three distinct types of lattice-preferred orientations of biotite grains were revealed in schlieren-delineated magmatic structures using the electron backscatter diffraction (EBSD) method. (1) Biotite basal planes (001) reorient from schlieren-subparallel near the schlieren base to schlieren-perpendicular in the upper part of the schlieren. Both orientations share subhorizontal N–S to NNE–SSW-trending a axes. (2) In some domains, the a axes are steep and at a high angle to the schlieren plane while the c axes plunge shallowly and rotate around an ill-defined a axis. (3) In other domains, the EBSD coincides with background magnetic fabric of the host granite revealed using the anisotropy of magnetic susceptibility (AMS) method: that is, the a axes plunge shallowly to the SE or NW while the c axes are subhorizontal and cluster around the NE–SW trend. In the porphyritic Jizera granite, Bohemian Massif, three distinct types of lattice-preferred orientations of biotite grains were revealed in schlieren-delineated magmatic structures using the electron backscatter diffraction (EBSD) method. (1) Biotite basal planes (001) reorient from schlieren-subparallel near the schlieren base to schlieren-perpendicular in the upper part of the schlieren. Both orientations share subhorizontal N–S to NNE–SSW-trending a axes. (2) In some domains, the a axes are steep and at a high angle to the schlieren plane while the c axes plunge shallowly and rotate around an ill-defined a axis. (3) In other domains, the EBSD coincides with background magnetic fabric of the host granite revealed using the anisotropy of magnetic susceptibility (AMS) method: that is, the a axes plunge shallowly to the SE or NW while the c axes are subhorizontal and cluster around the NE–SW trend. In the porphyritic Jizera granite, Bohemian Massif, three distinct types of lattice-preferred orientations of biotite grains were revealed in schlieren-delineated magmatic structures using the electron backscatter diffraction (EBSD) method. (1) Biotite basal planes (001) reorient from schlieren-subparallel near the schlieren base to schlieren-perpendicular in the upper part of the schlieren. Both orientations share subhorizontal N–S to NNE–SSW-trending a axes. (2) In some domains, the a axes are steep and at a high angle to the schlieren plane while the c axes plunge shallowly and rotate around an ill-defined a axis. (3) In other domains, the EBSD coincides with background magnetic fabric of the host granite revealed using the anisotropy of magnetic susceptibility (AMS) method: that is, the a axes plunge shallowly to the SE or NW while the c axes are subhorizontal and cluster around the NE–SW trend.
dcterms:title
Procesy v magmatu Grain-scale processes in actively deforming magma mushes: new insights from electron backscatter diffraction (EBSD) analysis of biotite schlieren in the Jizera granite, Bohemian Massif Grain-scale processes in actively deforming magma mushes: new insights from electron backscatter diffraction (EBSD) analysis of biotite schlieren in the Jizera granite, Bohemian Massif
skos:prefLabel
Grain-scale processes in actively deforming magma mushes: new insights from electron backscatter diffraction (EBSD) analysis of biotite schlieren in the Jizera granite, Bohemian Massif Procesy v magmatu Grain-scale processes in actively deforming magma mushes: new insights from electron backscatter diffraction (EBSD) analysis of biotite schlieren in the Jizera granite, Bohemian Massif
skos:notation
RIV/00025798:_____/08:00000257!RIV09-MZP-00025798
n4:aktivita
n14:P n14:Z
n4:aktivity
P(GA205/07/0783), Z(MSM0021620855), Z(MZP0002579801)
n4:cisloPeriodika
3-4
n4:dodaniDat
n5:2009
n4:domaciTvurceVysledku
n8:7257910 n8:8387699 n8:2387689
n4:druhVysledku
n15:J
n4:duvernostUdaju
n16:S
n4:entitaPredkladatele
n12:predkladatel
n4:idSjednocenehoVysledku
369586
n4:idVysledku
RIV/00025798:_____/08:00000257
n4:jazykVysledku
n10:eng
n4:klicovaSlova
Electron backscatter diffraction (EBSD), Granite, Magnetic susceptibility anisotropy, Pluton, Schlieren
n4:klicoveSlovo
n9:Electron%20backscatter%20diffraction%20%28EBSD%29 n9:Magnetic%20susceptibility%20anisotropy n9:Pluton n9:Schlieren n9:Granite
n4:kodStatuVydavatele
NL - Nizozemsko
n4:kontrolniKodProRIV
[CC4AB2871E4D]
n4:nazevZdroje
Lithos
n4:obor
n18:DB
n4:pocetDomacichTvurcuVysledku
3
n4:pocetTvurcuVysledku
3
n4:projekt
n7:GA205%2F07%2F0783
n4:rokUplatneniVysledku
n5:2008
n4:svazekPeriodika
106
n4:tvurceVysledku
Týcová, Patricie Žák, Jiří Verner, Kryštof
n4:wos
261680100008
n4:zamer
n6:MSM0021620855 n6:MZP0002579801
s:issn
0024-4937
s:numberOfPages
14