Xiazhuang uranium ore field

located in the Northern Guangdong province

is the most important uranium deposit collective region of granite type in China. Uranium resources in this area have the characteristics of superior metallogenic geological conditions and complex mineralization. In recent years

with the continuous depletion of hard rock type uranium resources in South China

it is urgent to find new areas and new types of uranium deposits.Based on the summary of the relationship between fault structure

magmatism and basic disk and uranium mineralization in the inductive area

combined with the surrounding rock alteration

mantle fluid and metallogenic source

Proposed the next step of prospecting in the Xiazhuang uranium ore field

that is

searching for the "trinity" area and "intersection type" uranium deposits composed of structure

magma and alteration

It provides the basis for the further work of ore field research and exploration in this area.