CAJ | 학술논문

该区在大地构造上位于Ⅱ级构造单元江南台隆中雪峰弧形构造带由NE向构造转为NEE向构造而形成的弧形转折部位。金矿床赋存于元古界板溪群（Ptbn）和元古界冷家溪群（Ptln）地层中，严格受元古界浅海相沉积的一套浅变质（碎屑）岩及断裂构造、热液蚀变控制。通过成矿条件综合分析，该区金成矿地质条件优越，具有较好的找矿潜力。
해구재대지구조상위우Ⅱ급구조단원강남태륭중설봉호형구조대유NE향구조전위NEE향구조이형성적호형전절부위。금광상부존우원고계판계군（Ptbn）화원고계랭가계군（Ptln）지층중，엄격수원고계천해상침적적일투천변질（쇄설）암급단렬구조、열액식변공제。통과성광조건종합분석，해구금성광지질조건우월，구유교호적조광잠력。
The area is located on the tectonic curved transition parts Ⅱ -class tectonic units the Jiangnan stacked platform uplift in Xuefeng arcuate tectonic belt into a NEE by NE trending tectonic formation of the constructor. The gold deposit occurrence in the Proterozoic Banxi Group (Ptbn) and Proterozoic Lengjiaxi (Ptln), strictly controlled by Fracture structure,hydrothermal alteration and the set of low-grade metamorphic (clastic) rocks in shallow marine deposition of the Proterozoic. Through comprehensive analysis of metallogenic conditions, that the area of gold metallogenic geological condition is superior, and has better prospecting potential.