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  • Investigations on a set of experimental models of highly viscous intrusions were carried out in order to study the internal strain pattern during vertical ascent and emplacement of granite intrusions. The strain pattern was determined by means of anisotropy of magnetic susceptibility resulting from the orientation of magnetite particles in a liquid plaster medium. The modelled intrusions show distinct fabrics reflecting the flow of a rheologically complex, non-Newtonian material. During the vertical growth of the intrusion, constrictional vertical fabrics are transposed into flattening fabrics, and along with the development of low-intensity fabric domains are passively transported upwards. Vertical growth takes place along subvertical thrust shear zones that satisfactorily explain the discordant magmatic fabrics in granites along intrusion sides.
  • Investigations on a set of experimental models of highly viscous intrusions were carried out in order to study the internal strain pattern during vertical ascent and emplacement of granite intrusions. The strain pattern was determined by means of anisotropy of magnetic susceptibility resulting from the orientation of magnetite particles in a liquid plaster medium. The modelled intrusions show distinct fabrics reflecting the flow of a rheologically complex, non-Newtonian material. During the vertical growth of the intrusion, constrictional vertical fabrics are transposed into flattening fabrics, and along with the development of low-intensity fabric domains are passively transported upwards. Vertical growth takes place along subvertical thrust shear zones that satisfactorily explain the discordant magmatic fabrics in granites along intrusion sides. (en)
Title
  • Fabric transpositions in granite plutons - an insight from non-scaled analogue modelling
  • Fabric transpositions in granite plutons - an insight from non-scaled analogue modelling (en)
skos:prefLabel
  • Fabric transpositions in granite plutons - an insight from non-scaled analogue modelling
  • Fabric transpositions in granite plutons - an insight from non-scaled analogue modelling (en)
skos:notation
  • RIV/67985530:_____/10:00337771!RIV11-AV0-67985530
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(KJB300120702), Z(AV0Z30120515)
http://linked.open...iv/cisloPeriodika
  • 1
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  • 258643
http://linked.open...ai/riv/idVysledku
  • RIV/67985530:_____/10:00337771
http://linked.open...riv/jazykVysledku
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  • analogue modelling; magmatic fabrics; granite intrusions; rheology; AMS (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • IN - Indická republika
http://linked.open...ontrolniKodProRIV
  • [C516FF0582AC]
http://linked.open...i/riv/nazevZdroje
  • Journal of the Geological Society of India
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http://linked.open...ichTvurcuVysledku
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 75
http://linked.open...iv/tvurceVysledku
  • Machek, Matěj
  • Kratinová, Zuzana
  • Kusbach, V.
http://linked.open...ain/vavai/riv/wos
  • 000277011800022
http://linked.open...n/vavai/riv/zamer
issn
  • 0016-7622
number of pages
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