About: A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic     Goto   Sponge   Distinct   Permalink

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Description
  • Geometrie násunových zlomů bradel Pavlovkých vrchů je typu ramp-flat-ramp, takže násunové plochy jsou stupňovité. Strmé úseky-rampy jsou indikovány pozicí antiklinál. (cs)
  • The Pavlov Hills formed by Jurassic limestones are a large outcroppe of bottom part of a large thrust sheet. The geometry is considerred to be ramp-and-flat, e.g. thrust faults have bedding-parallel and bedding-oblique sections. Ramps are marked by large anticlines.
  • The Pavlov Hills formed by Jurassic limestones are a large outcroppe of bottom part of a large thrust sheet. The geometry is considerred to be ramp-and-flat, e.g. thrust faults have bedding-parallel and bedding-oblique sections. Ramps are marked by large anticlines. (en)
Title
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic
  • Stupňovitá geometrie násunových zlomů v Pavlovských vrchách, Západní Karpaty, Česká republika (cs)
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic (en)
skos:prefLabel
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic
  • Stupňovitá geometrie násunových zlomů v Pavlovských vrchách, Západní Karpaty, Česká republika (cs)
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic (en)
skos:notation
  • RIV/00216224:14310/06:00017228!RIV08-MSM-14310___
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  • RIV/00216224:14310/06:00017228
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  • Pavlov Hills; tectonics; Jurassic (en)
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  • CZ - Česká republika
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  • 20
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  • Melichar, Rostislav
  • Poul, Ivan
http://linked.open...n/vavai/riv/zamer
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  • 1210-9606
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