Skarn formation is a significant geological process associated with the formation of ore deposits, particularly in the context of ore geology and industrial minerals. Skarns are metamorphic rocks that form at the contact zone between igneous intrusions, typically granitic, and carbonate sedimentary rocks such as limestone or dolomite. The process involves metasomatism, where the original rock undergoes chemical alteration due to the introduction of hot, mineral-rich fluids emanating from the cooling magma. The mineralogical composition of skarns is diverse and depends on the chemistry of both the intruding magma and the host carbonate