Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas

@article{Loucks2007MississippianBS,
  title={Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas},
  author={Robert G. Loucks and Stephen C. Ruppel},
  journal={AAPG Bulletin},
  year={2007},
  volume={91},
  pages={579-601}
}
  • R. LoucksS. Ruppel
  • Published 1 April 2007
  • Geology, Environmental Science, Geography
  • AAPG Bulletin
The Mississippian Barnett Formation of the Fort Worth Basin is a classic shale-gas system in which the rock is the source, reservoir, and seal. Barnett strata were deposited in a deeper water foreland basin that had poor circulation with the open ocean. For most of the basin's history, bottom waters were euxinic, preserving organic matter and, thus, creating a rich source rock, along with abundant framboidal pyrite. The Barnett interval comprises a variety of facies but is dominated by fine… 

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