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1)  channel sandbody description
河道砂体描述
1.
The successful techniques used fined structural interpretation, channel sandbody description and hydrocarbon recognition in Guantao Formation exploration such as coherent data,horizontal slice,3D visualization,joint inversion of seismic and well log,seismic attribute, instantaneous frequency and amplitude statistic, were analyzed systematically.
以该区馆陶组为研究对象,对在精细构造解释、河道砂体描述和含油气判识3个方面应用比较成功的相干体分析、水平切片分析、三维可视化分析、地震与测井联合反演、地震属性分析、瞬时频率以及振幅值统计等地球物理技术进行了系统总结,同时对埕东凸起北坡河道砂体进行了分类评价,共描述砂体104个,预测Ⅰ类砂体56个,Ⅱ类砂体24个。
2)  sand body description
砂体描述
1.
Therefore, the application of high-resolution thin-interbed inversion based on the model in sand body description and reservoir prediction has been studied.
为此,在该区开展了基于模型的高分辨率薄互层反演技术进行砂体描述和储层预测的研究。
3)  channel sand
河道砂体
1.
Control of base level cycles on channel sand geometry: A case study on Zao Ⅱ-Ⅲ reservoirs,Zaoyuan Oilfield;
基准面旋回对河道砂体几何形态的控制作用——以枣园油田孔一段枣Ⅱ—Ⅲ油组为例
2.
Identification of channel sand in three-dimensional seismic data;
河道砂体在三维地震资料解释中的识别
4)  channel sand body
河道砂体
1.
Description technique of channel sand body of upper Guantao formation in Feiyantan-laohekou area;
飞雁滩——老河口地区馆上段河道砂体描述技术
2.
Method of identifying oil-bearing ability in channel sand body;
河道砂体含油性判别方法
3.
Using seismic attributes to identify channel sand body;
应用地震属性分析技术刻画河道砂体
5)  channel sandbody
河道砂体
1.
Reservoir prediction technique of channel sandbody and its application in Daqing peripheral oilfields;
大庆外围油田河道砂体储层预测技术及应用
2.
An algorithm is put forward which can be used to trace the boundary of the channel sandbody in fluvial facies reservoir.
针对普通三角剖分算法构造三角网经常出现尖锐三角形的问题,提出了一种河流相储层河道砂体沉积相带自动追踪算法。
3.
Using the three-dimensional visualization software,we can accurately interpret structure and describe the forms of traps through showing the space of various attribute data of seismic data cube to composite fault and trace channel sandbody.
 利用三维可视化软件,通过对地震数据体各种属性数据的空间显示,进行断裂组合、河道砂体追踪,提高构造解释和圈闭形态描述的精度。
6)  river sandstone body
河道砂岩体
1.
Based on previous data, this paper sums up the reflection texture and the variety of amplitude of the river sandstone body in a d.
根据河道砂岩体主体的宽(w)与(h)高之比,河道砂岩体分为带状砂岩体(w∶h小于15)和席状砂岩体(w∶h大于15)。
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。
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