底流与重力流交互作用下的朵体沉积特征: 以东非鲁伍马盆地中新统为例*
刘钰星1,2,3,4, 陈宇航1,2,3,4, 范国章5, 李林5, 鲁银涛5, 左国平5, 曹全斌5, 丁群峰1,2,3

Sedimentary characteristics of lobes formed by interacting bottom currents and gravity flows: a case study from the Miocene in Rovuma Basin,East Africa
LIU Yuxing1,2,3,4, CHEN Yuhang1,2,3,4, FAN Guozhang5, LI Lin5, LU Yintao5, ZUO Guoping5, CAO Quanbin5, DING Qunfeng1,2,3
底流与重力流交互作用模式(据 Fonnesu et al ., 2020 ;有修改)