1) mid-channel bar
心滩坝
1.
Based on the former results about outcrop and modern deposition study,using dynamic and static data,the singe mid-channel bar was identified and anatomized.
以羊三木油田羊三断块馆二上段为例,提出了辫状河砂体储层构型的研究方法,即基于辫状河露头及现代沉积原形模型,应用动、静态资料在井间识别单个心滩坝砂体,进行井间构型预测,建立构型三维展布模型。
2) beach and bar
滩坝
1.
A study of beach and bar sands subtle reservoirs in western slope of Qinan sag;
歧南洼陷西斜坡滩坝砂隐蔽油气藏研究与评价
3) beach bar
滩坝
1.
Sedimentary characteristics and controlling factors of beach bars in the Upper Submember of the Fourth Member of the Shahejie Formation in the Lijin subasin;
利津洼陷沙四上亚段滩坝沉积特征及控制因素分析
2.
Sendimentary characteristics and model of tempestites-beach bar of upper section of the fourth member of Shahejie Formation in Boxing Sag
博兴洼陷风暴-滩坝沉积特征及模式
3.
The beach bar lithologic reservoir is small and hidden,its oil-water distribution is very complex,so reservoir identification and reservoir evaluation need more log data.
滩坝砂岩性油气藏规模小,隐蔽性强,其油水分布受多种因素的控制,需要更丰富的测井信息对其进行识别和评价。
4) Ertan arch dam
二滩拱坝
1.
Feedback analysis of material parameters of Ertan arch dam and its foundation rock;
二滩拱坝及坝基材料参数反馈分析
2.
Feedback analysis on temperature field of Ertan arch dam in operation period;
二滩拱坝运行期坝体温度场反馈分析
3.
Design and optimization study of the dam safety monitoring on the Ertan arch dam;
二滩拱坝安全监测设计及优化研究
5) Letan dam site
乐滩坝址
6) Longtan dam
龙滩大坝
补充资料：心滩
心滩
位于河心的浅滩，与复式环流作用有关。在河床突然加宽处，由于河水流速降低，在河底受两股相向的底流作用，于是，发生了侵蚀两岸，而在河床底部堆积，逐渐形成心滩。每当洪水期间，心滩就增大淤高，顶部覆盖了悬移质泥沙，发展成经常露于水面之上的江心洲，又称沙岛。江心洲比较稳定，但通常由于洲头不断冲刷，洲尾不断淤积，整个江心洲很缓慢地向下移动。由于心滩和江心洲的发展，使河流分汊，河床不稳定。在一定的条件下边滩和心滩可以互相转化，它们也都可能发展成河漫滩的一部分。我国黄河中下游河床宽浅，含沙量大，心滩和江心洲十分发育。
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