坦桑尼亚滨海盆地陆坡峡谷沉积特征及其控制因素*
陈宇航1,2,3, 姚根顺4, 邵大力4, 鲁银涛4, 吕福亮4, 曹全斌4, 唐鹏程4, 李仕芳5

Sedimentary characteristics and its controlling factors of continental slope canyons in Tanzania Coastal Basin
Chen Yu-Hang1,2,3, Yao Gen-Shun4, Shao Da-Li4, Lu Yin-Tao4, Lü Fu-Liang4, Cao Quan-Bin4, Tang Peng-Cheng4, Li Shi-Fang5
坦桑尼亚滨海盆地海底构造地貌与洋流分布 a—东非陆缘地貌及洋流及分布,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(据 Thiéblemont et al ., 2019 );b—坦桑尼亚陆缘海底构造;c—坦桑尼亚滨海盆地陆坡地形及洋流分布(据 Fonnesu et al ., 2020 );d—坦桑尼亚滨海盆地陆坡地貌三维可视化图