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Lou Zhanghua, Lu Qingmei, Cai Xiyuan, Dong Baiwan, Zhang Liqing. Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front[J]. Acta Sedimentologica Sinica, 1998, 16(4): 27-31.
Citation: Lou Zhanghua, Lu Qingmei, Cai Xiyuan, Dong Baiwan, Zhang Liqing. Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front[J]. Acta Sedimentologica Sinica, 1998, 16(4): 27-31.

Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front

  • Received Date: 1997-05-06
  • Rev Recd Date: 1997-09-24
  • Publish Date: 1998-08-10
  • At the geologic setting of shallow-water delta.distributary channels on plain palin can stretch into lake very long distance by sediment filling and the lake level frequent fluctuation.developping obvious subaqueous channel at wide shallow water delta front.At the same time,the lake level fluctuation,hydrodynamics,suchas channel,wave and offshore current,will change the distribution of sedimentary materials,and results in delta front sandbodies sheetlization,which mainly occurs in the subaqueous channel sandbodies.Along with the climate become more moist,the frequence and range of lake level fluctuation is also smaller,and the hydrodynamics reworks the distribution of sedimentary materials on delta front and sandbody sheetliation become weaker at the same time.
  • [1] 1 龚绍礼, 河南禹县早二叠世晚期浅水 三角洲沉 积和聚煤 环境.煤 田地质与勘探.1 986, 1 1 1( 2): 85~91

    2 夏文臣.鄂尔多斯盆地南部延安组水下分流河道型湖泊三角洲体 系的沉积构成.地球科学, 1 6( 2): 23~31

    3 李彦芳, 曲淑琴, 辛仁臣.松辽盆地三角洲与油气.北京: 石油工业 出版社.1 993.54~71

    4 Donalson A C.Pennsylvanian sedimentation cent ral A ppalaachians Spec Pap G eol S oc.A m.1 974, 1 48: 47~78

    5 Horme F C.Ferm F C.Baganz B P.Depositional models in c oal ex- plorat ion and minerplani ng i n Appalachian region.AA PG.62(1 2): 2 377~241

    6 H G 里丁主 编, 周明 鉴译.沉 积环境 和相.北 京科 学出 版社. 1 27~1 78
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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:  1997-05-06
  • Revised:  1997-09-24
  • Published:  1998-08-10

Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front

Abstract: At the geologic setting of shallow-water delta.distributary channels on plain palin can stretch into lake very long distance by sediment filling and the lake level frequent fluctuation.developping obvious subaqueous channel at wide shallow water delta front.At the same time,the lake level fluctuation,hydrodynamics,suchas channel,wave and offshore current,will change the distribution of sedimentary materials,and results in delta front sandbodies sheetlization,which mainly occurs in the subaqueous channel sandbodies.Along with the climate become more moist,the frequence and range of lake level fluctuation is also smaller,and the hydrodynamics reworks the distribution of sedimentary materials on delta front and sandbody sheetliation become weaker at the same time.

Lou Zhanghua, Lu Qingmei, Cai Xiyuan, Dong Baiwan, Zhang Liqing. Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front[J]. Acta Sedimentologica Sinica, 1998, 16(4): 27-31.
Citation: Lou Zhanghua, Lu Qingmei, Cai Xiyuan, Dong Baiwan, Zhang Liqing. Influence of Lake Level Fluctuation on Sandbody Shapes at Shallow—Water Delta Front[J]. Acta Sedimentologica Sinica, 1998, 16(4): 27-31.
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