The Polymetallic Mineralization Pattern of Iron,Manganese,Lead,Zinc,etc.,in the Manzhouli-Kerulen Metallogenic Belt
The Manzhouli-Kerulen Metallogenic Belt,situated in the Northeast Asian region,represents a significant concentration area for polymetallic mineral resources.This study introduces the geographical location and distribution of mineral resources within the belt and provides a detailed analysis of the three principal mineralization periods:Neoarchean to Paleoproterozoic,Late Paleozoic,and Mesozoic,with the most intense mineralization occurring during the Mesozoic.By examining the geological structural characteristics of the metallogenic belt,including regional structural controls on mineralization,characteristics of Mesozoic volcanic settings,and the influence of magmatic intrusions on mineralization,a regional mineralization model is delineated.It is highlighted that metal mineralization within the belt predominantly occurs during the Mesozoic and is characterized by polyphase and multistage processes.The findings of this research offer fresh insights into the region's mineralization and provide a scientific foundation for future geological exploration and resource prospecting endeavors.
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