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《Journal of Marine Sciences》 2006-03
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The present research situation and trend of submarine sand ridges geomorphology

WU Zi-yin~(1,2,3),CAO Zhen-yi~2,WANG Xiao-bo~2,ZHENG Yu-long~(1,2)(1.Second Institute of Oceanography,SOA,Hangzhou 310012,China;2.Laboratory of Submarine Geosciences,SOA,Hangzhou 310012,China;3.Department of Earth Sciences,Zhejiang University,Hangzhou 310028,China)  
Some study results and technologies of submarine sand ridges geomorphology are summarized,and several unfathomed issues of sand ridges on the eastern China seas are discussed in this paper.Currently,the search results from international famous periodicals(for example,Marine Geology and Sedimentary Geology) show that studies on the characteristics and causes of sand ridges are still the hot-topics of marine geology,and studies on the causes of radiate sand ridges off Jianggang,Jiangsu are the domestic focus.However,many topics of sand ridges on the north-central shelf of the ECS(East China Sea) are still in debate,such as the formation period(transgression or regression),deposit type(modern deposit,relict deposit or tidal deposit),deposition dynamics and deposition model.Although tidal currents play a key role on the development of sand ridges,ancient tidal currents are still not well studied and used quantificationally to analyze the causes of sand ridges in China.The latest multi-beam sounding data show that linear sand ridges are widely distributed on the outer shelf of the ECS,which are landward to the isobath of 60m and seaward to the water depth of 120m in the northeast and 150m in the southwest.The distributed scale of linear sand ridges on the shelf of the ECS is far wider than those from previous studies,and the three-dimensional structures and developing trends of linear sand ridges are different from that in the horn-shape area of Yangtze paleo-estuary,however,these sand ridges still have not been noticed fully and studied systematically.Finally,some advices for sand ridges study are put forward.The later studies on the elaborate structures and space-time distribution of sand ridges should be based on multi-kind data,such as the multi-beam sounding data,high-resolution single-channel seismic profile and the analyzing result of core and borehole etc.,studies on the evolution model and formation mechanism of sand ridges should be based on the results of ancient tidal currents and sea-level variations.
【Fund】: 国家自然科学基金资助项目(40506017)
【CateGory Index】: P737.2
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