Autogenic subaqueous mechanism for continental shelf formation associated with clinoform migration: dissolved salt, gravity-driven and wave-supported turbidity currents


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
Back to: Turbidity Currents and the Morphology and Stratigraphy They Create II