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通过对东闯特大型金矿床的重点研究，综合前人资料，对小秦岭金矿田矿床成因提出了新的认识。成矿流体由地幔流体交代演化而来，成矿物质主要来自上地幔和下地壳，成矿时代为晚燕山期，不同形式的拆离构造为成矿流体提供了运移通道和富集空间，其成因类型为幔源中高温热液金矿床。
Based on the key research on the East Chuang extra large gold deposit and synthesizing the previous data, a new understanding of the genesis of the deposit in the Xiaoqinling gold ore field is proposed. The ore-forming fluid is derived from the fluid exchange of mantle fluids. The metallogenic materials mainly come from the upper mantle and the lower crust. The mineralization age is late Yanshanian period. Different forms of detachment structures provide migration channels and enriched space for ore- Its genetic type is mantle-derived mid-high temperature hydrothermal gold deposit.