The Daxinganling area is located in the east-west Paleozoic paleo-Asian tectonic metallogenic field and the north-northeast to the Mesozoic-Cenozoic Eurasian Pacific west tectonic metallogenic domain strongly superimposed

complex and transform the site. In the southern section of Daxinganling Mountains

the ore-forming conditions are superior

the ore-forming period is more

the ore-forming intensity is large

and the deposit types are diverse. The evolution of the southern section of the Daxinganling Mountains was analyzed. The control of the mineralization is analyzed through the continental evolution

magmatic activity

continental crust evolution and polymetallic mineralization in the southern section of the Daxinganling Mountains.