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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(3): 29-32

Yang Dayuan, Xie Yuebo. Paleoflood Slack-Water Deposits[J]. Acta Sedimentologica Sinica, 1997, 15(3): 29-32.
Citation: Yang Dayuan, Xie Yuebo. Paleoflood Slack-Water Deposits[J]. Acta Sedimentologica Sinica, 1997, 15(3): 29-32.
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Paleoflood Slack-Water Deposits

  • 1 Dept. of Land & Ocean Science,Nanjing Univ.Nanjing 210093;

  • 2 Dept. of Hydrology & water Resources,Hehai Univ.Nanjing 210098

  • Received Date: 1996-08-30
  • Publish Date: 1997-09-10
  • Paleoflood study depends on the flood information drown from paleoflood deposits. Among those,the most valuable one is the paleoflood slack-water deposit. The paleoflood slack-water deposits at thedown reach from the Three Gorges of Yangtze River and from the Sanmen Gorge of the Yellow Riverwere burried and preserved on some terraces in gentle slope. They have slight stratification, which risesup at depositional termination, special grain size as well as the relative amount of every heavy mineral.The features above are also the important mark of looking for and ascertaining the paleoflood slack-wa-ter deposit for paleoflood study on different reaches in different drainage areas.
  • [1] O ' C onnor, J E, and webb, R H. Hydraulic modeling for pale-oflood analysis, in Baker, V R, Kochel, R C, and Patton, P C,eds, Flood Geomorphology: New York, John Wiley, 1988, 393～ 402.
    [2] Knox, J C. Larg e increases in flood magnitude in response tomodest chang e in climate, Nature, 1993, 361: 430 ～ 432.
    [3] O' Connor, J E, Ely, L L, Wohl, E E, Stevens, L E, Melis, T S,Kale, V S, and Baker, V R, 1994, A: 4500-year record of largefloods on the Colorado River in the Grand Canyon, Arizona,Jour Geology, 1994, 102: 1 ～ 9.
    [4] Baker, V R and Kochel, R C, Flood sedimentation in bedrockfluvial systens, in V R Baker, R C Kochel and P C Patton eds,Flood Geomorphology: New York, John wiley & sons, 1988,123 ～ 137.
    [5] Schmidt, J C, Recirculating flow and sedimentation in the Col-o rado River in Grand Canyon, Arizona, Jour, Geolog y, 1990,98: 709 ～ 724.
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Publishing history
  • Received:  1996-08-30
  • Published:  1997-09-10

Paleoflood Slack-Water Deposits

  • 1 Dept. of Land & Ocean Science,Nanjing Univ.Nanjing 210093;
  • 2 Dept. of Hydrology & water Resources,Hehai Univ.Nanjing 210098
  • Received Date: 1996-08-30
  • Publish Date: 1997-09-10

Abstract: Paleoflood study depends on the flood information drown from paleoflood deposits. Among those,the most valuable one is the paleoflood slack-water deposit. The paleoflood slack-water deposits at thedown reach from the Three Gorges of Yangtze River and from the Sanmen Gorge of the Yellow Riverwere burried and preserved on some terraces in gentle slope. They have slight stratification, which risesup at depositional termination, special grain size as well as the relative amount of every heavy mineral.The features above are also the important mark of looking for and ascertaining the paleoflood slack-wa-ter deposit for paleoflood study on different reaches in different drainage areas.

Yang Dayuan, Xie Yuebo. Paleoflood Slack-Water Deposits[J]. Acta Sedimentologica Sinica, 1997, 15(3): 29-32.
Citation: Yang Dayuan, Xie Yuebo. Paleoflood Slack-Water Deposits[J]. Acta Sedimentologica Sinica, 1997, 15(3): 29-32.
shu

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