摘要
渗透率是影响成矿热液运动的重要因素之一。通过系统分析和测定胶东望儿山金矿床成矿过程中不同成矿阶段的渗透率数据 ,建立了其分布模型 ,并将之与矿化强度模型进行对比 ,二者在空间上具有很强的耦合性 ,因此 ,渗透率模型可作为找矿的重要依据之一。
Permeability is one of the important factors which affect the ore formation. By analyzing the geologic characters and determining a lot of samples in Wangershan gold deposit, the mineralizing intensity distribution modeling and the time and space distribution patterns of permeability, which has coupling to each other in space, are established. Therefore the permeability of ore forming fluid is one of the indispensable marks for ore prospecting.
出处
《地质与勘探》
CAS
CSCD
北大核心
2001年第4期46-48,共3页
Geology and Exploration
基金
国家"九五"攻关项目 (96-914 -0 5 )
国土资源部定量预测和评价重点实验室基金联合资助
关键词
渗透率
矿化强度
耦合性
金矿床
成矿热液
找矿标志
permeability, intensity of mineralization, coupling, Wangershan gold deposit, eastern Shandong
