用数学地质的观点和方法处理野外地质工作所获得的大量数据,使用各种定量指标,可以对矿床形成过程和成矿机理作出有效地判断和估计。本文是在应用判别分析、聚类分析及硫同位素综合分析基础上,探讨“六一”硫铁矿床成矿作用规律的一个尝试。 Using mathematical geology perspectives and methods to deal with the large amount of data obtained in field geology work and using various quantitative indicators, we can effectively judge and estimate the formation process and the metallogenic mechanism. This paper is an attempt to discuss the metallogenic regularity of the “June 1” pyrite deposit on the basis of discriminant analysis, cluster analysis and comprehensive analysis of sulfur isotopes.