Eur. j. water qual.
 1981
DOI: 10.1051/water/19811201081
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Sur la teneur des eaux en sélénium en relation avec la présence de terrains détritiques de l'Eocène supérieur (formation de Brenne) : Exemples de sources de la basse vallée de la Creuse (départements de l'Indre et de la Vienne)

Pierre Saumande
1
,
Miguel Sarre2,
Claude Lorens3
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