摘要
分别对川西北哲波山微细浸染型金矿的构造、蚀变、矿化三者进行了详细的阐述 ,总结出该区构造活动的多发性和继承性制约着矿化的多阶段性和叠加性。矿化、蚀变的广度不能超越构造的限度。构造—蚀变—矿化三者之间的变化存在密切的正相关性。
Structure,alteration and mineralization of the Zheboshan fine disseminated gold deposit in northwest Sichuan are expounded in detail.To sum up control of multiphase and inherited tectonism on multistage and superimposed mineralization.Mineralization and alteration were controlled by structure.Structure,mineralization and alteration were in close relationship.
出处
《四川地质学报》
2000年第1期45-49,共5页
Acta Geologica Sichuan
关键词
微细浸染型金矿床
构造
蚀变
矿化
fine disemminated gold deposit,structure-alteration-mineralization,Zheboshan
