CAJ | 학술논문

长江中下游成矿带铜陵矿集区，长期以来为国内外研究的热点地区之一，但大都集中于研究Cu、Au、S、Fe等矿产，而铅锌矿的相关报道或科研工作相对较少。铜陵张家冲铅锌矿位于长江中下游成矿带繁昌盆地内，属次火山口控制的铅锌矿，是繁昌火山岩盆地内发现的第一个有色金属矿床，同时也是通过对盆地内硅化带的系统解剖发现的矿床，有着较高的科研和生产价值。笔者近年来组织了对该区的施工，提交（332+333）铅锌矿石资源量675.87×104t，Pb＋Zn金属量11.90×104t。本文旨在通过对该区铅锌矿地质特征、矿床成因、找矿标志及成矿规律等进行总结，进一步丰富该地区成矿模式和理论，为本区乃至整个繁昌盆地下步找矿提供参考和借鉴。
장강중하유성광대동릉광집구，장기이래위국내외연구적열점지구지일，단대도집중우연구Cu、Au、S、Fe등광산，이연자광적상관보도혹과연공작상대교소。동릉장가충연자광위우장강중하유성광대번창분지내，속차화산구공제적연자광，시번창화산암분지내발현적제일개유색금속광상，동시야시통과대분지내규화대적계통해부발현적광상，유착교고적과연화생산개치。필자근년래조직료대해구적시공，제교（332+333）연자광석자원량675.87×104t，Pb＋Zn금속량11.90×104t。본문지재통과대해구연자광지질특정、광상성인、조광표지급성광규률등진행총결，진일보봉부해지구성광모식화이론，위본구내지정개번창분지하보조광제공삼고화차감。
The Tongling mining camp in the mid-lower Yangtze River metallogenic zone has been one of hot spots for study at home and abroad for a long time, which mostly focused on minerals of Cu, Au, S and Fe, with less report on Pb and Zn. The Zhangjiachong Pb-Zn ore deposit, Tongling is situated in the Fanchang basin of the mid-lower Yangtze River metallogenic zone. Controlled by a subvolcanc crater, it is the first non-ferrous ore deposit ever found in the Fanchang volcanic rock basin, and is also a result of systematic analysis of silicified zone in the basin, bearing higher scientific research and production values. In recent years, the author organized work in the area and presented a resource 332+333of Pb-Zn ore at 675.87×104t, and Pb+Zn metal at 11.90×104t. This paper aimed to summarize geological features, ore genesis, ore-prospecting indicators and ore-forming pattern of Pb-Zn deposits in the area, further enrich metallogenic model and theory for the area and provide a reference for ore prospecting in the area and even the whole Fanchang basin in the future.