Sinian is one of the main periods of the formation of manganese deposits in
China. Sinian manganese deposits are mainly hosted in carbon-rich black sh
ale and siliceous shale formed during the Sinian interglacial period. The c
omposition of manganese ore is simple. The main ore mineral is manganiferou
s carbonates. The grade of manganese ore is about 16-25%, with Mn/Fe>S and
P/Mn=0.006-0.14. Based on the tectonic setting and geological and geochemic
al characteristics of manganese deposits, this paper discusses the process
of migration and concentration of manganese and ore-forming conditions of S
inian manganese deposits in China.