卡林型金矿床的构造和矿床特征分析

Structural and ore deposit characteristics of Carlin type gold deposit

卡林型金矿属于金矿床中非常重要的一种类型,是一种中低温、微粒以及浸染的热液矿床。地壳物质运动与地幔的不均衡将会使得元素进行再分配,导致矿物质多次的辅机。同时深大断裂以及沉积喷流等活动也促使了金矿的形成,与之相对应的岩浆活动则为成矿作用提供热源支持,这些活动共同促使卡林型金矿的形成。本文主要针对卡林型金矿床的构造和矿床的特征进行了详细的分析。

Carlin type gold deposit belongs to a very important type of gold deposit. It is a medium-low temperature, particulate and disseminated hydrothermal deposit. The movement of crustal materials and the imbalance of mantle will lead to the redistribution of elements, resulting in multiple auxiliaries of minerals. At the same time, deep and large faults and sedimentary jet activities also promoted the formation of gold deposits, and the corresponding magmatic activities were to enhance the power and heat source support for mineralization, which together promoted the formation of Carlin-type gold deposits. The structure and characteristics of Carlin type gold deposit are analyzed in detail in this paper.