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The Barnett Shale is a geological formation located in the Bend Arch-Fort Worth Basin. It consists of sedimentary rocks dating from the Mississippian period (354–323 million years ago) in Texas. The formation underlies the city of Fort Worth and underlies 5,000 mi² (13,000 km²) and at least 17 counties.

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  • Barnett Shale (en)
  • Schistes de Barnett (fr)
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  • Les schistes de Barnett (ou Barnett Shale pour les anglophones) sont une formation géologique située dans le nord du Texas, dans le bassin Bend Arch-Fort Worth. Elle est constituée de roches sédimentaires du Mississippien, des argilites datées de 354 à 323 millions d'années, qui s'étendent sous la région de la ville de Fort Worth et sur environ 13 000 km2 et au moins 17 comtés. Le géologue et paléontologue américain Wilbert Henry Hass (1906-1959) a travaillé sur l'étude des conodontes de la formation des schistes de Barnett en 1952. (fr)
  • The Barnett Shale is a geological formation located in the Bend Arch-Fort Worth Basin. It consists of sedimentary rocks dating from the Mississippian period (354–323 million years ago) in Texas. The formation underlies the city of Fort Worth and underlies 5,000 mi² (13,000 km²) and at least 17 counties. (en)
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  • Barnett Shale (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/BarnettShaleDrilling-9323.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Barnett_Shale_Map.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Barnett_Shale_lithology.gif
  • http://commons.wikimedia.org/wiki/Special:FilePath/Gas_Production_from_Barnett_2000-2013.png
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