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184矿床位于某复式折皱带复式向斜的西端(图1)。铀矿体赋存在震旦系上部灯影组陡山陀段第四层的一套硅质、炭质和白云质板岩中。矿化受层位和断层的控制,属于复成因矿床。矿床所在向斜北翼受断层破坏,除东南边缘的矿化层位部分出露地表以外,大部分工业矿体已被第三系红色砂砾岩掩盖,埋深不等,一般在200米以下。为了合理使用勘探工程,尽快地圈定第三系盖层下的矿化远景地段,缩短矿床
The 184 deposit is located at the western end of a compound fold belt syncline (Figure 1). The uranium ore body exists in a set of siliceous, carbonaceous and dolomitic slate in the fourth layer of the Upper Shade Formation of the Upper Sinian Dengying Formation. Mineralization is controlled by layers and faults and belongs to complex-genesis deposit. The northern slope of the syncline where the deposit is located is damaged by the fault. Most of the ore bodies in the ore body have been covered by the red sand and gravel rocks of the Tertiary except for the mineralized beds in the southeast margin, which are buried at depths below 200 meters. In order to make rational use of exploration projects, delineate mineralized prospect areas under the Tertiary cover as soon as possible to shorten the deposit