uranium rich 富铀的
uranium-rich massif 富铀岩体
uranium-rich horizon 富铀层位
uranium-rich black rock system 富铀黑色岩系
uranium rich black shale series 富铀黑色岩系
rich large uranium deposit 富大铀矿
rich uranium 富铀
rich uranium deposit 富铀矿床
The formation of uranium mineralization is considered as a result remobilization, migration and local concentration caused by preferential melting of the uranium-rich strata.
此类型矿床是富铀地层选择性熔融，并在此过程中导致铀的活化、转移和局部富集的结果。
The area has favourable regional metallogenic setting for sandstone uranium deposit. i. e uranium-rich basement, with arid to semiarid climate and desert to semiarid morphologic .
该区从区域上具有富铀基底、干旱—半干旱、沙漠—半沙漠的现代气候与地貌条件。
Nearshore shallow water environment, abundant terrestrial fine detritus, local reduction facies and zones are three cardinal conditions for the formation of uranium-rich sediments.
近岸的浅水条件，丰富的陆源细碎屑，局部的还原相带，是形成富铀沉积物的三个基本条件。
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