Ganshansi gold-antimony deposit in Shangzhou district

Shangluo city

Shaanxi province is located in the western section of Shaanxi-Henan gold-antimony metallogenic belt

in the Caotangou-Erlangping back-arc basin of the northern Qinling active continental margin

south of the Sanling fault and north of the Cai-Chuan fault. The deposit type is of medium-low temperature structural hydrothermal type

and the orebody is controlled by the near east-west structure. Based on regional metallogenic geology

ore deposit geology

ore body characteristics such as means to see yamadera gold antimony ore controlling factors

enrichment regularity and prospecting marks

ore deposit origin

such as make a comprehensive analysis

to see yamadera gold antimony mineralization mainly controlled by Cai-Chuan fault zone in the near east-west secondary structure

ore area silicide and carbonatization

silurian group of ore formation of lower palaeozoic era Anping group. The main ore-bearing lithologies are granulite

sericite

schist and marble.