刊名:Comptes Rendus de l'Academie des Sciences Series IIA Earth and Planetary Science
出版年:2001
出版时间:March 30, 2001
年:2001
卷:332
期:6
页码:371-378
全文大小:559 K
文摘
Deposits observed in cores collected on the south levee of the active middle Zaire deep-sea fan are fine-grained turbidites containing abundant thin silt laminae, alternated with clay laminae. Each sequence represents successive spillover of the dilute upper part of a continuous channelised turbidity current. Pulsatory overflows create a low velocity (0.1 m·s−1) overspill current on the levee with duration from a few days to a few weeks. Variations of the hydraulic regime within the overflow generate laminae.