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Li Fan. BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE[J]. Acta Sedimentologica Sinica, 1983, 1(3): 98-108.
Citation: Li Fan. BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE[J]. Acta Sedimentologica Sinica, 1983, 1(3): 98-108.

BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE

  • Received Date: 1982-09-13
  • Publish Date: 1983-09-10
  • Situated on the southern coast of Shangdoug Peninsula, Baishakou belongs to barrier lagoon coast. The bedforms and bedding structures of sediments in this region were investigated in 1981. The investigation shows that geomorpho-logical units, such as longshore barriers, lagoon, tidal delta, tidal channel and beach, have been developing there. In the coastal zone, there are asymmetric ripples, symmetric plane top ripples, interference ripples, backwash marks, permeate current borne rill marks, plane bed surface, surviving wave ripples, 'D' erosional holes, wind-borne ripples and so on. They have formed into a special distributional series of the sediment bedforms on the barrier lagoon coast.
  • [1] Reineck, H. E., I. B. Singh,著1977.陆源碎屑的沉积环境,18页。大庆油田l科学研究设计院等译。

    Alien, J. R. L.,1966, On bed forms and palcocurreuts, Sedimcniology,Vol. 5N0.6 p. 153-190。

    Clifton. H. E.,1976, Wave一formed sedimentary structures a conceptual model.Beach and Nearshore Sedimentation. p. 126一148.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1982-09-13
  • Published:  1983-09-10

BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE

Abstract: Situated on the southern coast of Shangdoug Peninsula, Baishakou belongs to barrier lagoon coast. The bedforms and bedding structures of sediments in this region were investigated in 1981. The investigation shows that geomorpho-logical units, such as longshore barriers, lagoon, tidal delta, tidal channel and beach, have been developing there. In the coastal zone, there are asymmetric ripples, symmetric plane top ripples, interference ripples, backwash marks, permeate current borne rill marks, plane bed surface, surviving wave ripples, 'D' erosional holes, wind-borne ripples and so on. They have formed into a special distributional series of the sediment bedforms on the barrier lagoon coast.

Li Fan. BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE[J]. Acta Sedimentologica Sinica, 1983, 1(3): 98-108.
Citation: Li Fan. BEDFORMS AND BEDDING STRUCTURES OF THE SEDIMENTS IN THE BAISHAKOU COASTAL ZONE[J]. Acta Sedimentologica Sinica, 1983, 1(3): 98-108.
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