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The Kupferschiefer (German for Copper Shale, also called Copper Slate) or Kupfermergel (Copper Marl), (T1 or Z1) is an extensive and remarkable sedimentary unit in Central Europe. The relatively monotonous succession is typically 30 to 60 centimetres (12 to 24 in) and maximum 2 metres (6.6 ft) thick, but extends over an area of 600,000 square kilometres (230,000 sq mi) across the Southern Permian Basin. The Kupferschiefer can be found in outcrop or in the subsurface straddling six countries, including parts of the southern North Sea. The lateral equivalent outcropping in England is called Marl Slate.

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  • Kupferschiefer (en)
  • Kupferschiefer (de)
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  • Der Kupferschiefer ist eine in Mitteleuropa vor allem im Untergrund weit verbreitete Gesteinsschicht oberpermischen Alters, die durch kalkhaltige, von organischer Substanz und fein verteiltem Pyrit dunkel gefärbte, feingeschichtete marine Tonsteine gekennzeichnet ist. Seinen Namen verdankt der Kupferschiefer dem Umstand, dass er lokal stark mit sulfidischen Kupfer-, Zink- und Bleierzmineralen und, an diese gebunden, einer Vielzahl weiterer Metalle (u. a. Silber) angereichert ist. (de)
  • The Kupferschiefer (German for Copper Shale, also called Copper Slate) or Kupfermergel (Copper Marl), (T1 or Z1) is an extensive and remarkable sedimentary unit in Central Europe. The relatively monotonous succession is typically 30 to 60 centimetres (12 to 24 in) and maximum 2 metres (6.6 ft) thick, but extends over an area of 600,000 square kilometres (230,000 sq mi) across the Southern Permian Basin. The Kupferschiefer can be found in outcrop or in the subsurface straddling six countries, including parts of the southern North Sea. The lateral equivalent outcropping in England is called Marl Slate. (en)
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  • Kupferschiefer (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Bundesarchiv_Bild_183-13175-0009,_Bergarbeiter,_Lore.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Coelacanthus_granulatus.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Thuringian_Forest_Geology.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/SMNK-PAL_2882.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/PalaeoniscusFreieslebenensis-NaturalHistoryMuseum-August23-08.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Geomap_Rhoen.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Geomap_Thur-Franc-Vogtl-SM.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kupferschiefer_Erzlineal.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Kupferschiefer_Fossilien.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mansfelder_Kupferlineal.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Palaeoniscus_freieslebeni.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pangea_-_260_Ma_-_with_Archosauromorpha_fossil_locations.jpg
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Kamsdorf_section.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Wodnika_striatula.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Elm_Asse_Dorm_geol.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Zechsteinmeer_europa.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Sphenobaiera_digitata.jpg
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