安徽省和县香泉萤石矿床地质特征及成因探讨OA

No.327 Unit of Bureau of Geology and Mineral Exploration of Anhui Province recently discovered a large-scale fluorite deposit in the Xiangquan area of He County.The deposit is hosted within a northeast-trending silicified breccia belt.Fluorite occurrences include micro-fine particles widely distributed in siliceous breccia,massive or stockwork fillings within the breccia matrix,and crystal clusters in cavities or fractures.Preliminary analysis suggests the deposit formed through early hydrothermal alteration followed by later hydrothermal filling superposition.Northeast-trending multi-stage faulting activities provided pathways for hydrothermal fluid migration and fluorite mineralization enrichment.Exploration markers for this deposit are clearly identifiable,indicating favorable exploration potential for analogous fluorite deposits in the region.