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Hello everyone! Today, we will take some time to learn about the Taebaeksan Mineral Belt, the treasure house of Korean geology and the largest producer of metallic minerals on the Korean Peninsula The fundamental reason why the Taebaeksan mineralization belt became a treasure trove of diverse mineral resources lies in the violent hydrothermal and chemical reactions between Paleozoic sedimentary rocks (especially carbonate rocks such as limestone) and granitic magma that intruded during the Mesozoic era. Magma-hydrothermal and skarn processes: Hydrothermal fluids originating from hot magma encountered Paleozoic limestone and calcareous rock layers, undergoing component exchange to form skarn deposits and hydrothermal ore bodies under high temperature and pressure. Zoning of deposits by distance: A distinct mechanism is observed where skarn ore bodies develop under high temperature and pressure conditions in areas adjacent to associated igneous rocks (magma), while hydrothermal vein deposits form as the temperature decreases with distance from the igneous rocks. Evolution of fluids by period: In the case of the Imok-ri-Nokjeon-ri-Sangdong area, high-temperature hydrothermal fluids containing tungsten (W) and molybdenum (Mo) were initially deposited mainly in the Sangdong deposit region. Subsequently, the gradually evolving fluid caused lead-zinc-copper (Pb-Zn-Cu±Mo±W) mineralization along the carbonate rock layers or fault zones within the Myobong Formation.

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