Research progress on architectural patterns and formation mechanisms of deep-water unidirectionally migrating channels
Zhou Wei1,2
不同沉积环境下次生环流样式及产物 A和A'—牵引流成因的曲流河(据 Armstrong,2012 ; Jobe et al ., 2016 ),河道内次生环流方向据 Bathurst等(1977) ;B和B'—浊流成因的深水弯曲水道(据 Abreu et al ., 2003 ),水道内次生环流方向据 Keevil 等(2006) ;C和C'—浊流与等深流交互作用成因的单向迁移水道及其次生环流样式(据 Gong et al ., 2016 , 2018 )