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1)  shore-shallow lacustrine sediment
滨浅湖沉积
1.
The shore-shallow lacustrine sediments of Upper Triassic in Central and South Sichuan Basin is enriched with ichnocoenosis, which consists of at least 6 ichnogenera, 8 ichnospecies, namely, Skolithos linearis, S.
川中-川南地区上三叠统滨浅湖沉积中产有丰富的动物遗迹化石,识别为3大类6属8种,包括Sko-lithos linearis,S。
2)  shore shallow lake depositional system
滨浅湖沉积体系
3)  littoral and very shallow sediments
滨浅湖相沉积
4)  Lakeshore sediments
湖滨沉积物
5)  shore-shallow lake facies
滨浅湖相
1.
Prediction of beach bar sand reservoirs of shore-shallow lake facies in Boxing subsag of Dongying sag;
东营凹陷博兴洼陷滨浅湖相滩坝砂岩储层预测
6)  shore-shallow lacustrine
滨浅湖
1.
The general sedimentary characteristics indicate that shore-shallow lacustrine deposits are the main types,while flood plain,delta and fan delta occurred mainly along the basin margin.
沉积相总体特征以滨浅湖沉积为主,而在研究区周缘则多发育河流泛滥平原、三角洲和扇三角洲沉积。
补充资料:丙午五月大雨五日不止镜湖渺然想见湖未废时
【诗文】:
朝雨暮雨梅正黄,城南积潦入车箱;镜湖无复鍼青秧,直浸山脚白茫茫。
湖三百里汉讫唐,千载未尝废陂防,屹如长城限胡羌,啬夫有秩走且僵,旱有灌注水何伤,越民岁岁常丰穰。
泆湖谁始谋不臧?使我妇子餍糟糠。
陵迁谷变亦何常,会有妙手开湖光。
蒲鱼自足被四方,烟艇满目菱歌长。



【注释】:
原题:丙午五月大雨五日不止镜湖渺然想见湖未废时有感而赋


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