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XUE Chun-ting. Sedimentary Record of Yellow River Delta Superlobe in 11~1099[J]. Acta Sedimentologica Sinica, 2008, 26(5): 804-812.
Citation: XUE Chun-ting. Sedimentary Record of Yellow River Delta Superlobe in 11~1099[J]. Acta Sedimentologica Sinica, 2008, 26(5): 804-812.
shu

Sedimentary Record of Yellow River Delta Superlobe in 11~1099

  • The Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao Shandong 266071

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  • Corresponding author: XUE Chun-ting
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-10-10
  • The Yellow River Delta superlobe in 111099 formed on a very shallow sea area. The thickness of the delta close to the coast line in 1855 is only 12 m. The delta front silt or interdistributary bay clayey silt accumulates on the prodelta. In the old delta deposits, the bioturbation structure can be observed, the mollusk shells are common, more foraminiferal tests and marine ostracod valves exist. They are different from those in North Jiangsu delta superlobe (11281855) and Modern Delta superlobe (since 1855). These indicate that the sedimentation rate in the old delta superlobe is lower than the other two younger delta superlobes and indirectly indicate the increasing erosion in the Loess Plateau.
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Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2008-10-10

Sedimentary Record of Yellow River Delta Superlobe in 11~1099

  • The Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao Shandong 266071
    Corresponding author: XUE Chun-ting
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-10-10

Abstract: The Yellow River Delta superlobe in 111099 formed on a very shallow sea area. The thickness of the delta close to the coast line in 1855 is only 12 m. The delta front silt or interdistributary bay clayey silt accumulates on the prodelta. In the old delta deposits, the bioturbation structure can be observed, the mollusk shells are common, more foraminiferal tests and marine ostracod valves exist. They are different from those in North Jiangsu delta superlobe (11281855) and Modern Delta superlobe (since 1855). These indicate that the sedimentation rate in the old delta superlobe is lower than the other two younger delta superlobes and indirectly indicate the increasing erosion in the Loess Plateau.

XUE Chun-ting. Sedimentary Record of Yellow River Delta Superlobe in 11~1099[J]. Acta Sedimentologica Sinica, 2008, 26(5): 804-812.
Citation: XUE Chun-ting. Sedimentary Record of Yellow River Delta Superlobe in 11~1099[J]. Acta Sedimentologica Sinica, 2008, 26(5): 804-812.
shu

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