|
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 Guozhang 5, LI Lin 5, LU Yintao 5, ZUO Guoping 5, CAO Quanbin 5, DING Qunfeng 1,2,3
|
|
东非鲁伍马盆地中新世早期朵体地震相特征 a—地震剖面图; b—地震剖面素描图 |
|
|
|
|
|