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.
2019, Vol. 36 
