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本文据成矿物质的来源,矿体所赋岩性、岩相,将嵩县萤石矿床定为产于酸性—中酸性岩浆接触带萤石矿床类型;从成矿规律来看80%矿脉产于燕山期晚期形成的花岗岩体内。控制萤石成矿作用的主要是岩石类型和断裂构造,断裂构造的控矿作用中主要是压(张)扭性断裂对成矿有利,且在嵩县境内,总体以NE主导方向控矿。
According to the sources of ore-forming materials, the lithology and lithofacies assigned to the orebody, the Songxian fluorite deposit is defined as the type of fluorite deposit produced in the acidic-intermediate acid magmatic contact zone. According to the metallogenic regularity, 80% In the late Yanshan granite body. The control of fluorite metallogenesis is mainly rock type and fault structure. In the ore-controlling action of fault structure, the compressive (Zhang) torsional fracture is favorable for metallogenetic mineralization. In Songxian, the ore-controlling is dominated by NE dominant direction.