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

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  • 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
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic (en)
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  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic
  • A ramp-and-flat geometry of thrust faults in the Pavlov Hills, Western Carpathians, Czech Republic (en)
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  • RIV/00216224:14310/06:00017228!RIV11-MSM-14310___
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  • RIV/00216224:14310/06:00017228
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  • Pavlov Hills; tectonics; Jurassic (en)
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  • Melichar, Rostislav
  • Poul, Ivan
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  • 14310
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