Abstract: The west of Xiangshan uranium ore field is an important metallogenic area of Xiangshan ore
field , and the hydrogeological conditions belong to simple to medium type. Based on mining practice ,
combined with the comparative study of exploration and mining and the test data of pumping water from
several boreholes , it was shown that most of the ore bodies in the west of Xiangshan are located below
the local erosion datum , and the hydraulic connection between river water and groundwater is poor.
Water filling does not pose a threat to the deposit. The geological structure is complex , but there is no
strong water conductivity structure , the groundwater recharge condition is good. The water pressure is
high , but the main water-bearing zone-the structure ( secondary structure ) fissure water-bearing
zone , which affects the water filling of the deposit is week in aquosity , the estimated water inflow of
the mine pit is small. However , during the course of mining , the monitoring should be strengthened to
judge the change of water discharge in time to ensure the safety of production.
黄少钦,周良卿. 相山铀矿田西部主要含矿构造水文地质特征[J]. 世界核地质科学, 2019, 36(02): 91-97.
HUANG Shaoqin,ZHOU Liangqing. The hydrogeology characteristics of the major ore-hosting
structure in the west of Xiangshan uranium ore field. , 2019, 36(02): 91-97.