利用粒度参数分析石岛湾海岸泻湖的沉积环境THE UTILIZATION OF GRAIN SIZE PARAMETERS TO ANALYSE THE COASTAL LAGOON SEDIMENTARY ENVIRONMENT OF SHIDAO BAY
刘仲衡,吴锦秀,张亚民,李洪文,王少波,刘胜利,孙运良
摘要(Abstract)：
<正> 海岸泻湖和三角洲一样部位于海陆之间过渡的海岸地带,但泻湖是平行海岸延伸的水体,它以砂坝或障壁岛与外海相隔开,并经潮流(汐)通道与它相连接,海(湖)水和沉积物质在潮流的帮助下或进入泻湖,或流入外海。因此,泻湖沉积就属于这种环境下的一种特殊的沉积。
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作者(Author): 刘仲衡,吴锦秀,张亚民,李洪文,王少波,刘胜利,孙运良
DOI: 10.16441/j.cnki.hdxb.1983.02.009
参考文献(References)：
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- [6] 宋天锐等 1978． 我国南方的两种现代滨海沉积类型.地质学报.第二期第115-123页.
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