Metallogenic Mechanism of the Galinge Polymetallic Iron Skarn Deposit, Qiman Tagh Mountains, Qinghai Province

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The thesis explores the metallogenetic mechanisms of the Galinge skarn deposit through a multidisciplinary approach, integrating tectonics, geochemistry, and petrology. It details the multistage growth of skarn minerals, emphasizing how their compositions reflect hydrothermal fluid evolution. Key aspects include skarn zonation and the role of volatile-rich minerals like tourmaline and hastingsite. Additionally, it outlines the regional tectonic-magmatic history, providing insights into metallogenic principles that can aid in field prospecting.