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主要讨论火山岩和相关侵入岩地区金矿的形成机制问题．把整个成矿系统分为成矿热流体体系和控矿环境两部分．把热流体分为近地表和高侵位两类岩浆－热流体体系；把控矿环境划分为火山中心、高侵位岩体和复合在其上的构造破碎带等６类控矿系统，全面分析了各类控矿系统内具有共性特征的物质－能量综合场，指出金矿的形成过程也是成矿热流体体系与控矿环境之间进行物质、能量交换的过程；金的局部富集不仅取决于体系与环境之间、体系内部各因素之间和外部各控矿条件之间的耦合程度，而且也与金元素大范围、长时间充分补给和小范围局部富集的时、空条件有关．作者把这套认识概括为“内外多元耦合、四维局部富集”的成矿机制
It mainly discusses the formation mechanism of gold deposits in volcanic rocks and related intrusive rocks. The whole metallogenic system is divided into ore-forming thermal fluid system and ore-controlling environment in two parts. The thermal fluid is divided into two types of magmatic-thermohydrodynamic system near surface and high emplacement. The ore-control environment is divided into six types of ore-control systems such as volcanic center, high-intrusion rock mass and structural fracture zone compounded on it. It is pointed out that the formation process of gold deposits is also the process of material and energy exchange between the ore-forming thermal fluid system and the ore-control environment. The local enrichment of gold not only Depends on the coupling between the system and the environment, between the various elements of the system and between the external control conditions, but also with the time and space conditions of the gold element in a large area, full supply for a long time and local enrichment in a small area . The author summarizes this understanding as a “mineralization mechanism of multiple internal and external coupling, four-dimensional local enrichment”