OS12A:
Turbidity Currents and the Morphology and Stratigraphy They Create II


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Session ID#: 57626

Session Description:
Turbidity currents constitute a major mechanism for sculpting the submarine and sublacustrine world. They excavate deep canyons, and can run out over 1000 km on deepwater fans. They create rhythmic topography such as mud waves, cyclic scour holes and meandering channels. Fan channels in particular can have levees over 50 m high. We solicit contributions across a wide spectrum in regard to a) turbidity current dynamics, including plunging, self-acceleration and self-channelization; b) associated morphology including meandering, bedforms, canyons and fans; and c) stratigraphy across the full range of deep-sea architecture. In this session we honor Henry Pantin, who was a major innovator in turbidity current dynamics, particularly in regard to self-acceleration.
Primary Convener:  Robert Michael Dorrell, University of Hull, Energy and Environment Institute, Hull, United Kingdom
Convener:  Jeffrey Peakall, University of Leeds, Leeds, LS2, United Kingdom
Primary Liaison:  Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States
Chairs:  Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States, Jim Best, University of Illinois at Urbana Champaign, Department of Earth Science & Environmental Change, Champaign, United States, Jeffrey Peakall, University of Leeds, Leeds, LS2, United Kingdom and Robert Michael Dorrell, University of Hull, Energy and Environment Institute, Hull, United Kingdom
OSPA Liaison:  Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States

Cross-Listed:
  • EP - Earth and Planetary Surface Processes
Index Terms:

1824 Geomorphology: general [HYDROLOGY]
3002 Continental shelf and slope processes [MARINE GEOLOGY AND GEOPHYSICS]
3022 Marine sediments: processes and transport [MARINE GEOLOGY AND GEOPHYSICS]
3045 Seafloor morphology, geology, and geophysics [MARINE GEOLOGY AND GEOPHYSICS]

Abstracts Submitted to this Session:

Toshiki Iwasaki, Civil Engineering Research Institute for Cold Region, Hokkaido, Japan and Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States
Tao Sun1, Fabien J Laugier1, Rebecca Caldwell2, Ashley Harris3 and Morgan Sullivan4, (1)Chevron Energy Technology Company, Earth Science Dept., Houston, TX, United States, (2)Chevron Energy Technology Company, Houston, United States, (3)Chevron Corporation Houston, Energy Technology Company, Houston, TX, United States, (4)Chevron Energy Technology Company, Earth Science Department, Houston, TX, United States
Amit Kumar, ExxonMobil Upstream Research Company, Houston, TX, United States and Thomas C Halsey, ExxonMobil Upstream Research Company, Spring, TX, United States
Steven Y. J. Lai, National Cheng Kung University, Dept. of Hydraulic and Ocean Engineering, Tainan, Taiwan, David Amblas, CRG Marine Geosciences, Dept. of Earth and Ocean Dynamics, University of Barcelona, Barcelona, Spain and Thomas P Gerber, Equinor, Research and Technology, Austin, TX, United States
Hajime Naruse, Kyoto University, Division of Earth and Planetary Sciences, Kyoto, Japan and Sojiro Fukuda, Kyoto University, Kyoto, Japan
Norihiro Izumi, Hokkaido University, Sapporo, Japan, Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States and Rossella Luchi, University of Illinois at Urbana Champaign, Urbana, IL, United States
Gary Parker, University of Illinois at Urbana Champaign, Earth Science and Environmental Change & Civil and Environmental Engineering, Urbana, United States

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