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上东坑地区地处诸广岩体东南部,百顺断陷带中段,铀矿化广泛。区内岩浆活动频繁,构造发育,铀矿化明显,好点带多,是一个富大铀矿产出地区。区内分布有大型361富矿床、小型235矿床和一系列铀矿点,矿化依产出围岩可划分为硅化带型和辉绿岩型。区内具有非常有利于铀成矿的区域地质背景、岩体条件和构造条件,仍然具有一定的找矿前景。
The upper Dongkeng area is located in the southeastern part of the Zhuang-Guang massif and the middle part of the Baishun rift zone with a wide range of uranium mineralization. Magmatic activity in the region is frequent, tectonic development, uranium mineralization obvious, with a good point, is a rich uranium-producing areas. Large 361 rich ore deposits, small 235 deposits and a series of uranium deposits are distributed in the area. Silicification zones and diabase types can be classified according to the ore-bearing rocks. The regional geological background, rock mass conditions and tectonic conditions that are very favorable to uranium metallogenesis in the area still have some prospecting potential.