The O Grao turbidite system: architectural and depositional interpretations from outcrop and well data (Middle Eocene, Ainsa Basin, Spain)


The O Grao turbidite system is part of the infill of the piggy-back stage of evolution of the Ainsa basin, and a portion of the Ainsa Slope Complex. The outcrops are on the flanks of the Buil syncline, on a 15 km long... [ view full abstract ]


  1. Pau Arbués (Universitat de Barcelona)
  2. Marco De Matteis (Universitat de Barcelona)
  3. Patricia Cabello (Universitat de Barcelona)
  4. Martí Burcet (Universitat de Barcelona)
  5. Timothy Demko (ExxonMobil Upstream Research Company)
  6. Vitor Abreu (Consultant)

Topic Area

Topics: Turbidites and deep marine systems


MS16 » Turbidite and deep sea deposits II (11:00 - Wednesday, 25th May, KARAM 2)

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