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通过对贵州省盘县陇英大地金矿床金矿矿区地层、构造、矿体特征、矿石特征等方面的研究,初步认为该区金矿体主要产于峨眉山玄武岩组一段及二段玄武质熔岩底部,受断层旁侧的节理、裂隙控制金矿体在断层破碎带内呈顺层和穿层两种状态产出。此外,通过对贵州省盘县地区峨眉山玄武岩底部和玄武岩之间的凝灰岩中的微细粒浸染型金矿床的研究,认为此类金矿的区域分布受控于峨眉山玄武岩及其边缘凝灰岩分布区;区域性控矿构造如扬子陆块西南缘的深部构造和区域性深大断裂,控制了金矿成矿及矿体的形成和分布,局部性构造决定了矿体的空间分布及产出特征。最后提出在该区寻找相同类型金矿的找矿标志及找矿远景。
By studying the stratigraphy, tectonics, ore body characteristics and ore characteristics of the gold deposits in the Longying Dadian gold deposit in Panxian, Guizhou, it is preliminarily believed that the gold orebody in this area is mainly produced at the bottom of the first and second basaltic lavas of the Emei Shan basalt group , By the side of the fault joints, fracture control gold ore body within the fault rupture zone was stratified and through two layers of state output. In addition, through the study of fine-grained diagenetic gold deposits in the tuff between the bottom of Emeishan basalts and the basalt in Panxian area, Guizhou, it is considered that the regional distribution of these gold deposits is controlled by the Emeishan basalts and their marginal tuff distribution areas; Sex control structures such as the deep structure and deep deep faults in the southwestern margin of the Yangtze block control the formation and distribution of gold ore deposits and ore bodies. The local structure determines the ore body spatial distribution and output characteristics. Finally, it is proposed to find prospecting prospect and prospecting prospect of the same type of gold deposit in this area.