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The Kupferschiefer (German for Copper Shale, Copper Schist or 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 cm and maximum 2 m thick, but extends over an area of 600000 km2 across the Southern Permian Basin. The Kupferschiefer can be found in outcrop or

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