【摘要】 在成矿构造环境研究基础上,指出滇东南晚古生代-中生代沉积盆地属裂陷构造盆地性质。该裂陷构造盆地是本区金矿赋存的重要空间，也是它们的成矿场所。本区存在多个金的高背景层位，金矿成矿受地层、岩性、构造变形作用、岩浆作用等因素的综合控制，这些因素在不同区段、不同时段的耦合梯度差是造成本区金矿成矿与否的关键条件。基于成矿控制因素的综合分析，建立了区域成矿模式，强调只有耦合梯度高的区段才可能有金的工业矿体出现，并进一步讨论了本区金矿的找矿方向。更多还原

【Abstract】 Based on the study of metallotect environment,it is pointed that the southeastern Yunnan Basin of late Palaeozoic－ Mesozoic era belongs to a taphrogeosyncline basin.The basin is not only a gold ore－ hosted space,but also a metallogenic locus.There are many horizons with high gold－ bearing content in the area.Metallogensis of gold deposits are controlled by stratum,rock type,and structural deformation as well as magmatism.The coupling gradient of these gold ore－ controlling factors is a key condition that gold deposits are formed,or not.According to the above analyses,the authors have established a regional metallogenic model for gold deposits,and emphasized that industral gold bodies can form only under sectors of high couplied gradient of gold ore－ controlling factors. Meanwhile,the prospecting directions of gold deposits are discussed.更多还原