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The Csehbánya Formation is a geological formation in the Transdanubian Mountains of Veszprém County, Hungary. The formation dates to the Late Santonian (around 85-84 million years ago) of the Late Cretaceous. It represents a floodplain environment as opposed to the swampy lacustrine environment of the simultaneous , though there is complete overlap in terms of fauna. It underlies the , and laterally transitions to the Ajka Coal Formation.

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dbo:abstract
  • Souvrství Csehbánya (doslova "český důl") je geologickou formací na území západního Maďarska (župa Veszprém). Stáří sedimentů činí asi 85 až 84 milionů let, jedná se tedy o usazeniny z období pozdní křídy (geologický věk santon). (cs)
  • The Csehbánya Formation is a geological formation in the Transdanubian Mountains of Veszprém County, Hungary. The formation dates to the Late Santonian (around 85-84 million years ago) of the Late Cretaceous. It represents a floodplain environment as opposed to the swampy lacustrine environment of the simultaneous , though there is complete overlap in terms of fauna. It underlies the , and laterally transitions to the Ajka Coal Formation. (en)
  • La formación geológica es una formación en Hungría cuyos estratos datan del Cretácico superior. Los restos de dinosaurios se encuentran entre los fósiles que se han recuperado de la formación.​ (es)
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  • Csehbánya Formation (en)
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dbp:otherlithology
dbp:overlies
  • Unconformity with Upper Triassic Main Dolomite Formation and Upper Cretaceous Nagytárkány Bauxite Formation (en)
dbp:period
  • Santonian (en)
dbp:prilithology
dbp:region
dbp:thickness
  • Varies, but up to (en)
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dbp:underlies
  • Jákó Marl Formation, localized unconformity with Eocene Iharkút Conglomerate present in some areas (en)
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gold:hypernym
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  • 47.24 17.64
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  • Souvrství Csehbánya (doslova "český důl") je geologickou formací na území západního Maďarska (župa Veszprém). Stáří sedimentů činí asi 85 až 84 milionů let, jedná se tedy o usazeniny z období pozdní křídy (geologický věk santon). (cs)
  • The Csehbánya Formation is a geological formation in the Transdanubian Mountains of Veszprém County, Hungary. The formation dates to the Late Santonian (around 85-84 million years ago) of the Late Cretaceous. It represents a floodplain environment as opposed to the swampy lacustrine environment of the simultaneous , though there is complete overlap in terms of fauna. It underlies the , and laterally transitions to the Ajka Coal Formation. (en)
  • La formación geológica es una formación en Hungría cuyos estratos datan del Cretácico superior. Los restos de dinosaurios se encuentran entre los fósiles que se han recuperado de la formación.​ (es)
rdfs:label
  • Csehbánya Formation (en)
  • Souvrství Csehbánya (cs)
  • Formación Csehbánya (es)
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