1) tidal lagoon
潮成泻湖
2) lagoon tidal flat
泻湖潮坪
3) barrier lagoon tidal inlet system
沙坝-泻湖-潮汐通道体系
4) lagoon
[英][lə'ɡu:n] [美][lə'gun]
泻湖
1.
Based on the stratigraphic, structural features and the types of ore deposits in Lingshi, it is concluded that the gypsum was deposited in supratidal lagoons.
根据灵石石膏矿区的地层、构造特征，矿床特征及矿石类型等对矿床的成因进行了分析探讨，认为该矿床是在潮上泻湖中沉积而形成。
2.
Sedimentological studies of coal-bearing member of Ceshui Fomation inLengshuijing coal mine indicate that it is sediments of depositional system of barrier is-land-lagoon and shows vertical sequence from regression to transgression,Coalaccumulation is influenced by depositional environments in a great degree.
本文依据对冷水江矿区测水组含煤段的沉积环境分析，提出该段为障壁岛──泻湖体系的沉积、垂向上表现为海退序列─—海进序列。
3.
The Zhanjiang Bay can be regarded as a tidal inlet system of drowned valley lagoon type.
湛江湾是一溺谷—泻湖型的潮汐通道系统，着重讨论了围海造地与该系统的关系，特别指出１９５８年的南三岛的联围，使湛江湾扩大了纳潮面积，完善了潮汐通道系统。
6) Hougang lagoon
后港泻湖
1.
On the basis of the field investigation in Hougang lagnoon and nearby Meye island area,this paper discusses the formation and evolution of Hougang lagoon which formed after the post-glacial maximum transgression,according to the data of core SO2 such as size of grain,~(14)C data,forminifera etc.
根据荣成后港泻湖和镆铘岛周围地区的勘察及S02孔岩芯样品的粒度1、4C、有孔虫等分析资料阐明了该泻湖的形成和演化过程,其形成于冰后期最大海侵之后(约7KaB。
补充资料：迎潮送潮辞·送潮
【诗文】：
潮西来兮又东下，日染中流兮红洒洒。汀葭苍兮屿蓼枯，
风骚牢兮愁烟孤。大几望兮微将晦翳，睨瀛溶兮敛然而退。
爱长波兮数数，一幅巾兮无缨可濯。帆生尘兮楫有衣，
怅潮之还兮吾犹未归。
【注释】：
【出处】：
全唐诗：卷621-22
潮西来兮又东下，日染中流兮红洒洒。汀葭苍兮屿蓼枯，
风骚牢兮愁烟孤。大几望兮微将晦翳，睨瀛溶兮敛然而退。
爱长波兮数数，一幅巾兮无缨可濯。帆生尘兮楫有衣，
怅潮之还兮吾犹未归。
【注释】：
【出处】：
全唐诗：卷621-22
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条