. . "000295534200005" . "RIV/67985831:_____/11:00367548!RIV12-AV0-67985831" . "209055" . . . "Ullemeyer, K." . . . . . "18"^^ . "7" . "International Journal of Earth Sciences" . . "1437-3254" . . "4"^^ . . . "1"^^ . . . "DE - Spolkov\u00E1 republika N\u011Bmecko" . "M\u00FCller, A." . "RIV/67985831:_____/11:00367548" . . "Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms" . "10.1007/s00531-010-0590-6" . "100" . . "The lattice-preferred orientation (LPOs) of two late-Variscan granitoids, the Meissen monzonite and the Podles\u00ED 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\u20136 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 Podles\u00ED 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." . "Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms" . "[1663DD8DBC17]" . . "Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms"@en . "Leiss, B." . . "The lattice-preferred orientation (LPOs) of two late-Variscan granitoids, the Meissen monzonite and the Podles\u00ED 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\u20136 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 Podles\u00ED 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."@en . "Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms"@en . "neutron diffraction; lattice-preferred orientation; shape-preferred orientation; magmatic flow; Podles\u00ED granite; Meissen massif"@en . . "Z(AV0Z30130516)" . "Breiter, Karel" .