About: Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)     Goto   Sponge   NotDistinct   Permalink

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  • Fold-and-thrust belts occur worldwide, have formed in all eras of geological time, and are widely recognized as the most common mode in which the crust accommodates shortening. Much current research on the structure of fold-and-thrust belts is focused on structural studies of regions or individual structures and on the geometry and evolution of these regions employing kinematic, mechanical and experimental modelling. In keeping with the main trends of current research, this title is devoted to the kinematic evolution and structural styles of a number of fold-and-thrust belts formed from Palaeozoic to Recent times.
  • Fold-and-thrust belts occur worldwide, have formed in all eras of geological time, and are widely recognized as the most common mode in which the crust accommodates shortening. Much current research on the structure of fold-and-thrust belts is focused on structural studies of regions or individual structures and on the geometry and evolution of these regions employing kinematic, mechanical and experimental modelling. In keeping with the main trends of current research, this title is devoted to the kinematic evolution and structural styles of a number of fold-and-thrust belts formed from Palaeozoic to Recent times. (en)
Title
  • Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)
  • Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic) (en)
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  • Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic)
  • Polyphase deformation of the Variscan accretionary wedge: an example from the southern part of the Moravian Karst (Bohemian Massif, Czech Republic) (en)
skos:notation
  • RIV/00216224:14310/11:00054655!RIV12-MSM-14310___
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  • S, Z(MSM0021622412)
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  • 221272
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  • RIV/00216224:14310/11:00054655
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  • Moravian Karst Moravosilezian zon tectonics thrust fold (en)
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  • [58ED2260033A]
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  • London
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  • Special publications 349
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  • Kinematic Evolution and Structural Styles of Fold-and-Thrust Belts
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http://linked.open...ichTvurcuVysledku
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http://linked.open...UplatneniVysledku
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  • Kalvoda, Jiří
  • Melichar, Rostislav
  • Rez, Jiří
http://linked.open...n/vavai/riv/zamer
number of pages
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  • Geological Society London
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  • 978-1-86239-320-2
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  • 14310
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