Is there a fluvial response to the Palaeocene-Eocene Thermal Maximum in the Bighorn Basin?


Records of the Paleocene-Eocene Thermal Maximum (PETM) have been well documented in continental sediments of the Bighorn Basin, NW Wyoming. Previous studies have concentrated on the detailed documentation of sedimentation... [ view full abstract ]


  1. Amanda Owen (University of Aberdeen)
  2. Alena Ebinghaus (University of aber)
  3. Adrian Hartley (University of Aberdeen)
  4. David Jolley (University of Aberdeen)
  5. Gary Weissmann (University of New Mexico)

Topic Areas

Topics: Fluvial depositional systems , Topics: Sedimentary signatures of global changes


MS10 » Sedimentary signature of Global Changes I (11:30 - Tuesday, 24th May, KARAM 2)

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