The metallogenic geological characteristics of Luoshan deposit are studied

and its genesis and prospecting potential are analyzed. Based on the metallogenic theory of granite type uranium deposit

study the lithology

structure

wall rock alteration

geophysical anomaly and ore body

it is considered that Luoshan deposit belongs to hydrothermal uranium deposit.Uranium mineralization is strictly controlled by fracture structure and the contact zone between mixed granite and Xiankou rock mass. Uranium mineralization is divided into two stages

but closely related to alkali metasomatism. The distribution of surface geophysical anomalies is obviously controlled by structures

which indicates the deep concealed uranium mineralization. In the next step

geological work should be strengthened around the blank area between zone 2 and zone 4 and zones 5

6

8 and 9

which is expected to expand the scale of the deposit to medium and large-scale.