折腰山、小铁山矿床的成因认识

来源期刊：中南大学学报(自然科学版)1983年第1期

论文作者：陈兰桂

文章页码：50 - 57

关键词：小铁山矿床； 折腰山； 成因认识； 含铜黄铁矿； 石英钠长斑岩； 火山热液矿床； 石英脉； 微量元素组合； 矿床地质特征； 成矿阶段

摘    要：本文根据矿床地质特征及矿物包裹体研究等方面的资料,综合分析后认为:折腰山、小铁山矿床(工业矿体)成因为火山热液矿床。

Abstract: Baiyinchang is one of the important copper base areas in China. There has always been an argument about the genesis of its copper deposit, the solution of which is of great significance both in theory and in practice. In accordance with the data related, such as that of the geologic characteristics of the deposits, that of the characteristics of the enclosure of the minerals, the author made a thorough analysis and an all-round summerization, consi- dering that Zheyaoshan and Xiaotieshan ore deposits are hydrothermal type, and their formation is related to postvolcanic activities.