论文部分内容阅读
114矿床位于南岭伟向构造带大东山-贵东亚带,粤北山字型西翼,系产于碳酸盐岩断裂带中的中低温热液充填交代单铀矿床。铀矿体主要产于石炭纪和二叠纪地层中,受新华夏系北西向张性构造复合早期构造带控制。
114 deposit is located in the Dadongshan-Guidong belt in the Weixiang tectonic belt of Nanling and the western wing of the Shannxiigou type in the north of Guangdong. It is a low-temperature hydrothermal hydrothermal filling metasomatic single-uranium deposit in the carbonate fracture zone. Uranium ore bodies are mainly produced in the Carboniferous and Permian strata and are controlled by the NWHX NWZ composite early tectonic belt.