First direct observations linking confined supercritical turbidity currents to their depositional architecture and facies characteristics
Sophie Hage1, Matthieu Cartigny2, John E Hughes Clarke3, Michael Andrew Clare4, Esther Sumner5, Stephen Michial Hubbard6, Peter Talling7, Gwyn Lintern8, Cooper Stacey9, Mark E. Vardy10, James Hunt4, Daniela Vendettuoli11, Miwa Yokokawa12, Jamie Lee Hizzett4, Age Jan Vellinga4 and María Azpiroz4, (1)Universite Paris-Saclay, Geosciences, Paris, France, (2)University of Durham, Department of Geography, Durham, United Kingdom, (3)Center for Coastal and Ocean Mapping Joint Hydrographic Center, Durham, NH, United States, (4)National Oceanography Centre, Southampton, United Kingdom, (5)University of Southampton, National Oceanography Centre, Southampton, United Kingdom, (6)University of Calgary, Department of Earth, Energy and Environment, Calgary, AB, Canada, (7)University of Durham, Earth Sciences and Geography, Durham, United Kingdom, (8)Geological Survey of Canada, sidney, BC, Canada, (9)Natural Resources Canada, Sidney, BC, Canada, (10)National Oceanography Centre, Southampton, Marine Geosciences, Southampton, United Kingdom, (11)University of Southampton, & NOC, Southampton, United Kingdom, (12)Osaka Institute of Technology, Information Science & Technology, Hirakata, Japan
