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YU Bin, ZHANG Shu-cheng, WANG Shi-ge. A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China[J]. Acta Sedimentologica Sinica, 2005, 23(4): 559-565.
Citation: YU Bin, ZHANG Shu-cheng, WANG Shi-ge. A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China[J]. Acta Sedimentologica Sinica, 2005, 23(4): 559-565.

A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China

  • Received Date: 2005-01-11
  • Rev Recd Date: 2005-04-13
  • Publish Date: 2005-12-10
  • Goose Foot River is located in the south of Qionghai Lake, Sichuan, China. Huge sediment was carried into Qionghai Lake by debris flows and floods of Goose Foot River in recent 15 years. The sediment deposited in the lake and formed an underwater levee in the lake. The underwater levee is 2km in length, 200m ( along south coast)to 600m ( along north coast) in width and the average 2m in height. A channelwas found in the lake in 2003 and it was connected with the fan of river. Itwill be helpful for the research of deposition in lake and deep sea. Research on turbidity currents, especially high density turbidity currentswill have specialmeaning not only for the geomorphology of lake and deep sea, but also for the seeking the hydrocarbon in lake and deep sea.
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    4 余斌,王士革,章书成,孟国才. 鹅掌河泥石流对四川邛海影响的初步研究[J].湖泊科学,2005,(01).

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    14 Schwenc K T,Speiβ V,Hübscher C,Breitzke M. Frequent channel avulsions within the active channel - levee system of the middle Bengal Fan-an exceptional channel - levee development derived from Parasound and Hydrosweep data[J].Deep-Sea Research Part 2:Topical Studies in Oceanography,2003.1023-1045.

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  • Received:  2005-01-11
  • Revised:  2005-04-13
  • Published:  2005-12-10

A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China

Abstract: Goose Foot River is located in the south of Qionghai Lake, Sichuan, China. Huge sediment was carried into Qionghai Lake by debris flows and floods of Goose Foot River in recent 15 years. The sediment deposited in the lake and formed an underwater levee in the lake. The underwater levee is 2km in length, 200m ( along south coast)to 600m ( along north coast) in width and the average 2m in height. A channelwas found in the lake in 2003 and it was connected with the fan of river. Itwill be helpful for the research of deposition in lake and deep sea. Research on turbidity currents, especially high density turbidity currentswill have specialmeaning not only for the geomorphology of lake and deep sea, but also for the seeking the hydrocarbon in lake and deep sea.

YU Bin, ZHANG Shu-cheng, WANG Shi-ge. A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China[J]. Acta Sedimentologica Sinica, 2005, 23(4): 559-565.
Citation: YU Bin, ZHANG Shu-cheng, WANG Shi-ge. A Prelim inary Study on the Deposition of Turbidity Currents in Qionghai Lake, Sichuan, China[J]. Acta Sedimentologica Sinica, 2005, 23(4): 559-565.
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