2) 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）。
3) channel sandstone type uranium deposit
河道砂岩型铀矿
1.
Analysis on depositional system and discussion on ore-formation conditions of channel sandstone type uranium deposit--taking Dongsheng area,Ordos Meso-Cenozoic basin as an example;
沉积体系分析与河道砂岩型铀矿成矿条件讨论——以鄂尔多斯中新生代盆地东胜地区为例
4) basal-channel sandstone-type uranium deposits
底河道砂岩型铀矿
1.
On the base of the deposit researching,it is concluded that basal-channel sandstone-type uranium deposits with roll front must need two conditions: the first is the metallogenic sandbody has better stratified,connectivity and permeability;the second is the stratigraphic frame must be have better water-resisti.
通过对该铀矿地质特征的研究,认识到发育卷状矿体的底河道砂岩型铀矿必须具备两大条件:其一是成矿砂体条件,即砂体要有较好的成层性、连通性和渗透性;其二是地层结构条件,即砂体必须存在较好的上、下隔水岩层。
6) paleochannel-type sandstone-hosted uranium deposit
古河道型砂岩铀矿
1.
On the base of the application of transient electromagnetic technique of paleochannel-type sandstone-hosted uranium deposits in Tengchong region of Yunan Province, This paper analyses the detect example.
可为我国其它地区的古河道型砂岩铀矿勘查提供借鉴。
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