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霍什布拉克铅锌矿所在区域位于天山褶皱系中的天山南脉地槽褶皱带,卡拉铁克-萨儿明泥盆纪-石炭纪弧盆的西南侧。由于卡拉铁克大断裂的不断活动,导致泥盆系呈断块隆起,泥盆系发生层间滑动,产生一些逆掩断层。矿体和含矿地层的产状一致。主矿体的矿石具有条带状、纹层状构造,矿石中大量发育霉球状、管状和环带状生物结构,显示出层控、热水沉积成因的特点。
The Hohrabuluo-Pb-Zn deposit is located in the Tianshan South vein geosynclinal fold belt in the Tianshan fold system and on the southwestern side of the Devonian-Carboniferous Arc of the Catharat-Sargent Mingfang. Due to the continuous activities of the Great Karakrishnan Fault, the Devonian was fault-block uplifted and the Devonian strata slipped to produce some overthrust. Ore body and ore-bearing formation consistent. The ore of the main orebody has a banded and laminar structure, and the moldy, tubular and ring-shaped biological structures are extensively developed in the ore, showing the characteristics of stratiform control and hot water deposition.