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<sup>*</sup>

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 Yuxing^1,^2,^3,⁴, CHEN Yuhang^1,^2,^3,⁴, FAN Guozhang⁵, LI Lin⁵, LU Yintao⁵, ZUO Guoping⁵, CAO Quanbin⁵, DING Qunfeng^1,^2,³

东非鲁伍马盆地位置及洋流分布(据 Breitzke et al ., 2017 ; Fonnesu et al ., 2020 ; Chen et al ., 2020 ;有修改) NEMC(Northeast Madagascar Currents)=马达加斯加东北洋流; EACC(East African Coastal Current)=东非沿岸流; MC(Mozambique Current)=莫桑比克海岸流; NADW(North Atlantic Deep Water)=北大西洋底流