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Sedimentary processes in Zenisu deep-sea channel revealed by side-scan imagery
- Journal of Oceanology and Limnology Vol. 23, Issue 4, Pages: 368-375(2005)
- Affiliations：
1. Institute of Oceanology Chinese Academy of Sciences
2. Graduate School of the Chinese Academy of Sciences
3. Ocean Research Institute University of Tokyo
- Author bio：
- Funds：
DOI：10.1007/BF02842679
CLC：-
Published：2005
- Accepted：
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Shiguo, W., Junhua, G. & Hidekazu, T. Sedimentary processes in Zenisu deep-sea channel revealed by side-scan imagery., Chin. J. Ocean. Limnol. 23, 368–375 (2005). https://doi.org/10.1007/BF02842679
摘要
Abstract
Side-scan sonar data collected by Cruises 99-09 Leg 2 and 00-06 Leg 1 of R/V Yokosuka were used to reveal the sedimentary processes in Zenisu deep-sea channel. The middle and lower segments of the channel are rich in turbidite and other debrite deposits. By high-resolution imaging
three sedimentary processes were distinguished with distinct acoustic features. 1. Slumps and slides occur with contrasting backscatter
rough surface textures
blockings
and acoustic shadows at head walls. They are very extensive and often in lobate form downslope. 2. Debris flow has uniform
general medium backscatter
sometimes showing marbling/lineation in lobate form. 3. Turbidity current is characterized by low backscatter confined to the channel as acoustic signal is attenuated. Regional tectonics must be the dominating factor that controls deposition pattern in this area.
关键词
Keywords
references
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