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湘中清水塘矿四定位于断裂带中。从矿脉形态、矿化类型和形式、矿液组分、矿化多阶段性等方面，论述了断裂控矿作用与矿液致裂成矿特点。地洼期构造岩浆活动，伴随矿液的充填压裂，形成矿田内主要矿脉、矿脉中心部位出现条带致密块状矿石，矿脉两端为网脉、细脉、分枝脉、脉的旁侧发育着羽列脉，在矿脉中常见有中石构造，可拼接角砾状矿石和断裂桥构造。显示出控矿断裂经历了从韧性到脆性递进变形作用过程。
Qingzhongtang deposit four located in the fault zone. From the aspects of vein morphology, mineralization type and form, ore fluid composition and multi-stage mineralization, the ore-fracturing and ore-forming characteristics are discussed. The magmatic activity in the Diwa period was accompanied by the filling and fracturing of the ore fluid, forming the main vein in the ore field. The dense ore blocks appeared in the central part of the veins. The veins at both ends were reticular veins, veins, branches and veins Developed with feather veins, common in the veins of the stone structure, can be spliced brecciated ore and fault structure of the bridge. It shows that the ore-controlling faults experienced a gradual deforming process from ductile to brittle.