1) the flood-over lake sedimentary
洪水-漫湖沉积
2) Flooded-lake facies
洪水漫湖
3) flood-overlake
洪水-漫湖
1.
It was showed,by cores observation,grain size analysis,logging data and electron microscope observation in Jiyang Paleogene depression,that the sediment of flood-overlake was controlled by ephemeral flood because the lake was shallow and the weather was dry-half dry.
结果表明,济阳坳陷在孔一段到沙四段沉积早期处于湖盆裂陷初期,沉积作用明显受季节性洪水注入影响,在东营、惠民两凹陷形成洪水-漫湖沉积体系。
4) flood-lake facies
洪水-漫湖相
5) floodwater deposit
洪水沉积
1.
Studying on a river-course-style lake,Wujindan lake in Xinghua, the author collect late holocene deposit samples 20-280cm in the means of undergroumd, analyse these samples observation with eyes,grain size,clay mineral observation bytx-ray,mineral magnetic,the content of B, gromdomg samples, then but forward the marks of floodwater deposit in the samples.
选择兴化市乌巾荡（湖泊），在湖滨采集地表２０ｃｍ至２８０ｃｍ的晚全新世沉积层连续样品，经物理鉴定后，又进行粘土、粘土矿物Ｘ衍射、磁化率、硼含量，部分岩芯磨片镜下观测等多元测试分析，提出了乌巾荡湖相沉积层中鉴别洪水沉积的标志与初步结论。
6) flood deposit
洪水沉积物
补充资料：河道洪水演进(见河道洪水演算法)
河道洪水演进(见河道洪水演算法)
neaao non郎hUi河道洪水演进yanJ县n 见河道洪水演算法。
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