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Flow processes and sedimentation in unidirectionally migrating deep‐water channels: From a three‐dimensional seismic perspective
Author(s) -
Gong Chenglin,
Wang Yingmin,
Steel Ronald J.,
Peakall Jeff,
Zhao Xiaoming,
Sun Qiliang
Publication year - 2016
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/sed.12233
Subject(s) - geology , sinuosity , flow (mathematics) , channel (broadcasting) , geomorphology , amplitude , sedimentary depositional environment , accretion (finance) , petrology , geometry , structural basin , telecommunications , physics , mathematics , quantum mechanics , computer science , astrophysics
Three‐dimensional seismic data were used to infer how bottom currents control unidirectional channel migration. Bottom currents flowing towards the steep bank would deflect the upper part of sediment gravity flows at an orientation of 1° to 11° to the steep bank, yielding a helical flow circulation consisting of a faster near‐surface flow towards the steep bank and a slower basal return flow towards the gentle bank. This helical flow model is evidenced by the occurrence of bigger, muddier (suggested by low‐amplitude seismic reflections) lateral accretion deposits and gentle channel wall with downlap terminations on the gentle bank and by smaller, sandier (indicated by high‐amplitude seismic reflectors) channel fills and steep channel walls with truncation terminations on the steep bank. This helical flow circulation promotes asymmetrical depositional patterns with dipping accretion sets restricted to the gentle bank, which restricts the development of sinuosity and yields unidirectional channel migration. These results aid in obtaining a complete picture of flow processes and sedimentation in submarine channels.