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韧性剪切带型金矿床作为重要金矿床类型之一,对其进行深入研究具有重要的理论和实际意义。以索尔巴斯陶金矿床与哈图金矿床为例,对韧性剪切带型金矿床地质特征进行概括和总结。韧性剪切带型金矿床与其赋存的韧性剪切带往往具有形成时间上的滞后效应,矿体严格受韧性剪切带的控制,但多分布在韧性剪切带的后期脆性断裂中。剥蚀程度比较低,长期演化的造山带环境是寻找韧性剪切带型金矿床的战略方向。
Ductile shear zone type gold deposits, as one of the important gold deposit types, have important theoretical and practical significance for further study. Taking the Solbarust gold deposit and Hatu gold deposit as examples, the geological characteristics of the ductile shear zone gold deposit are summarized and summarized. The ductile shear zone type gold deposit and its occurring ductile shear zone tend to have a time lag effect. The ore body is strictly controlled by the ductile shear zone but distributed in the late brittle fracture of the ductile shear zone. The eroded degree is relatively low. The long-term evolution of the orogenic belt environment is the strategic direction for finding ductile shear zone type gold deposits.