摘要
宝兴厂矿区地质构造复杂,成矿条件有利。区内北东向响水断裂带是主要的控岩和控矿构造。三类金矿床分别在斑岩成矿期、热液成矿期和表生成矿期成生。文中建立相应的成矿模式。
The geological structure of Baoxingchang orefield is complicated and the metallogenetic condition is advantageous.The northeastward Xiangshui fault zone in this area is the main rock-control and ore-control structure.There are 3 types of Au deposit,which are formed separately in the porphyry metallogenetic period,hydrothermal metallogenetic period,epigenetic metallogenetic period and have their corresponding metalloge-netic models.
引文
[1]何明勤、杨世瑜等,滇西小龙潭—马厂箐地区铜金多金属矿床地质地球化学及成因研究[M],北京:地质出版社,2004.
[2]葛良胜、王文成、李汉光等,滇西北富碱岩体与金矿成矿[M],北京:地震出版社,2005.
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