南岭成矿带矿床地质特征及成因探讨

Geological characteristics and genesis of deposits in Nanling metallogenic belt

寒洞矿区地处位于南岭成矿带信丰—全南复背斜东翼、于山构造成矿带的南端,矿体发育于北东向破碎带中,圈出1条规模较大矿体,属中低温热液充填型矿床。本文重点阐述矿床的地质特征,探讨矿床成因,以期对矿区进一步探矿和外围找矿有所启发。

Handong mining area is located in the east wing of Xinfeng QUANNAN complex anticline and the south end of Yushan structural metallogenic belt in Nanling metallogenic belt.The orebody is developed in the NE trending fracture zone,and a large-scale ore body is delineated.It belongs to medium low temperature hydrothermal filling type deposit.This paper focuses on the geological characteristics of the deposit and discusses the genesis of the deposit,with a view to enlighten the further exploration and peripheral prospecting in the mining area.