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以往对铀矿床的构造研究主要反映在断裂的几何形态、力学性质以及与铀矿化的空间关系的描述,断裂构造作用中的显微构造及同步地球化学作用与铀成矿关系研究则报导很少。
The previous studies on the tectonics of uranium deposits mainly reflect the geometry and mechanical properties of fractures, the description of the spatial relationship with uranium mineralization, the microstructures in synsedimentary structures and the relationship between synchrotron geochemistry and uranium mineralization less.