相山铀矿田热结构特征与成矿关系——以邹家山矿床为例

银涌兵, 李海英, 卢腾, 韩飘平, 孔德旭, 万环环, 庞文静, 吴志春

Relationships between thermal structure characteristics and mineralization of the Xiangshan uranium ore field:A case study of the Zoujiashan deposit

YIN Yong-Bing, LI Hai-Ying, LU Teng, HAN Piao-Ping, KONG De-Xu, WAN Huan-Huan, PANG Wen-Jing, WU Zhi-Chun

图5 研究区地温与矿体关系剖面 1—下白垩统鹅湖岭组碎斑熔岩;2—下白垩统打鼓顶组流纹英安岩;3—断裂构造;4—地层界线;5—工业矿体;6—地温等值线(℃);7—蚀变带范围;8—钻孔

Fig.5 Profile of relationship between ground temperature and ore body in the study area 1—lower Cretaceous ehuling formation porphyry lava; 2—rhyolitic dacite of daguding formation in lower Cretaceous; 3—fault structure; 4—stratigraphic boundary; 5—industrial ore body; 6—geothermal isoline(℃); 7 —alteration zone range; 8—drill hole