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This document summarizes a study that examines how creeping slope failure influences turbidity current behavior based on two outcrop examples from the Eocene slope succession in the Ainsa Basin of Spain. In the examples, mass-transport deposits continued to creep contemporaneously with turbidity current deposition and bypass. Structures in the mass-transport deposits were either extensional and parallel to flow, or compressional and perpendicular to flow. This influenced the routing and deposition of turbid

Author

Sebastian Kaempfe

Language

EN