About: Lattice-preferred orientations of late-Variscan granitoids derived from neutron diffraction data: implications for magma emplacement mechanisms     Goto   Sponge   NotDistinct   Permalink

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  • 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. (en)
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 (en)
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 (en)
skos:notation
  • RIV/67985831:_____/11:00367548!RIV12-AV0-67985831
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
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  • Z(AV0Z30130516)
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  • 7
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  • 209055
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  • RIV/67985831:_____/11:00367548
http://linked.open...riv/jazykVysledku
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  • neutron diffraction; lattice-preferred orientation; shape-preferred orientation; magmatic flow; Podlesí granite; Meissen massif (en)
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  • DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV
  • [1663DD8DBC17]
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  • International Journal of Earth Sciences
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http://linked.open...v/svazekPeriodika
  • 100
http://linked.open...iv/tvurceVysledku
  • Breiter, Karel
  • Leiss, B.
  • Müller, A.
  • Ullemeyer, K.
http://linked.open...ain/vavai/riv/wos
  • 000295534200005
http://linked.open...n/vavai/riv/zamer
issn
  • 1437-3254
number of pages
http://bibframe.org/vocab/doi
  • 10.1007/s00531-010-0590-6
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