Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments

KONG Xianghuai LIU Jian DU Yuansheng WEN Chun XU Gang

KONGXianghuai, LIUJian, DUYuansheng, WENChun, XUGang. Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments[J]. 海洋学报英文版, 2011, (1): 47-58. doi: 10.1007/s13131-011-0090-y
引用本文: KONGXianghuai, LIUJian, DUYuansheng, WENChun, XUGang. Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments[J]. 海洋学报英文版, 2011, (1): 47-58. doi: 10.1007/s13131-011-0090-y
KONG Xianghuai, LIU Jian, DU Yuansheng, WEN Chun, XU Gang. Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments[J]. Acta Oceanologica Sinica, 2011, (1): 47-58. doi: 10.1007/s13131-011-0090-y
Citation: KONG Xianghuai, LIU Jian, DU Yuansheng, WEN Chun, XU Gang. Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments[J]. Acta Oceanologica Sinica, 2011, (1): 47-58. doi: 10.1007/s13131-011-0090-y

Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments

doi: 10.1007/s13131-011-0090-y
基金项目: The National Natural Science Foundation of China under grant No. 40876034; the National Basic Research Program under grant No. 1212010611401.

Seismic geomorphology of buried channel systems in the western South Huanghai Sea: retrodiction for paleoenvironments

  • 摘要: Quantitative morphologic analysis of shallowly buried, dendritic channel systems in the continental shelf off the abandoned Huanghe River (Yellow River) mouth has been made based on interpretation of high resolution seismic profiles, with the attempt to estimate the paleo-hydrologic parameters when the incised-channels formed, then assess the paleoenvironment. The results indicate that the buried channel systems were formed about 44 cal ka BP when the shelf was subaerially exposed and subsequently drowned and filled during the Holocene transgression with the sea level rise continuously. The study area has experienced the processes from fluvial and estuarine to fully marine.
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  • 收稿日期:  2010-04-28
  • 修回日期:  2010-12-17

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