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  • Complex structure and paleostress studies along eastern apical domain of the Moravosilesian zone in flysh foredeep and coal-bearing molasse of Upper Silesian Coal Basin carry out. Three progressive deformation stages and mechanisms could be define. We suggested model of Variscan orogeny orocline, which explains complex tectonic and deformation history of this most eastward promontory of European Variscan orogeny. The Brunovistulian foreland terrane played an essential role in bending of the orocline.
  • Complex structure and paleostress studies along eastern apical domain of the Moravosilesian zone in flysh foredeep and coal-bearing molasse of Upper Silesian Coal Basin carry out. Three progressive deformation stages and mechanisms could be define. We suggested model of Variscan orogeny orocline, which explains complex tectonic and deformation history of this most eastward promontory of European Variscan orogeny. The Brunovistulian foreland terrane played an essential role in bending of the orocline. (en)
Title
  • Tectonic setting and deformation history of the Upper Silesian Coal Basin
  • Tectonic setting and deformation history of the Upper Silesian Coal Basin (en)
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  • Tectonic setting and deformation history of the Upper Silesian Coal Basin
  • Tectonic setting and deformation history of the Upper Silesian Coal Basin (en)
skos:notation
  • RIV/61989100:27350/01:00001246!RIV/2002/MSM/273502/N
http://linked.open.../vavai/riv/strany
  • 10
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  • Z(MSM 273500007)
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  • 698377
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  • RIV/61989100:27350/01:00001246
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  • Tectonics, Coal, Deformatin, Upper Silesian Coal Basin (en)
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  • [5830EDC85015]
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  • Praha
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  • Praha
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  • Abstracts of 9th Coal Geology Conference
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  • Grygar, Radomír
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number of pages
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  • Univerzita Karlova v Praze. Přírodovědecká fakulta
http://localhost/t...ganizacniJednotka
  • 27350
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