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Relationship between the characteristics of landforms and sediments as well as the plume front in the Hangzhou Bay
作者姓名:Feng Yingjun  Li Yan  Li Bogen
作者单位:Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
基金项目:This work is supported by both Grant-4860244 from the National Natural Science Foundation of China and Grant-188011 from the Zhejiang Provincial Natural Science Foundation
摘    要:Sedimentary environments in the Hangzhou Bay are introduced by a three-subregional landform pattern and a sedimentation map with six major sedimentation types. The geographic setting, sediment transportation and sedimentation in different subregions are discussed with sediment grain parameters. Sedimentary basin suffering from effect of plume front can be identified by the fine sediments with median ( Mdφ ) 7φ-8φ, clay content 30% - 40% and silt 60% - 70%. Sediment transportation along the plume front seems not to be a direct effect on sedimentary formation of the shoals fringing the south coast of the Hangzhou Bay.

收稿时间:1992/2/23 0:00:00
修稿时间:1992/5/20 0:00:00

Relationship between the characteristics of landforms and sediments as well as the plume front in the Hangzhou Bay
Feng Yingjun,Li Yan,Li Bogen.Relationship between the characteristics of landforms and sediments as well as the plume front in the Hangzhou Bay[J].Acta Oceanologica Sinica,1993,12(1):133-144.
Authors:Feng Yingjun  Li Yan and Li Bogen
Institution:Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China
Abstract:Sedimentary environments in the Hangzhou Bay are introduced by a three-subregional landform pattern and a sedimentation map with six major sedimentation types. The geographic setting, sediment transportation and sedimentation in different subregions are discussed with sediment grain parameters. Sedimentary basin suffering from effect of plume front can be identified by the fine sediments with median (Mdφ) 7φ-8φ, clay content 30%-40% and silt 60%-70%. Sediment transportation along the plume front seems not to be a direct effect on sedimentary formation of the shoals fringing the south coast of the Hangzhou Bay.
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