深入阐述“绿色凝灰岩区”和“非绿色凝灰岩区”的区域构造演化特征以及与成矿的关系。
The regional tectonic evolution characteristics of "green tuff region" and "Non green tuff region" and their relationship with uranium mineralization are elaborated in depth.
受盆地构造演化特征的影响，盆地内铀矿化存在两种类型，即潜水氧化带型和局部性层间氧化带型。
Features of tectonic evolution resulted in the development of two type uranium mineralizations in the basin, I e. phreatic oxidation and local interlayer oxidation types.
对盐构造的研究集中于演化特征对构造变形的控制作用；
The study on salt tectonic is concentrated on the structural transformation controlled by the evolution characters.
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