晚阶段具梳状构造的石英-碳酸盐细脉形成于伸展引张环境。
The late stage quartz-carbonate veinlets, with comb structure, are likely formed in an extensional tectonic environment.
矿床受近南北向断裂构造控制，矿体以脉状、透镜状、豆芽状赋存于这些断裂破碎带中。
Mineral deposit controlled by north and south faulted structure, mineral body exist in faulted structure with lenticular style, vein style and sprouted style.
银矿体受隐爆角砾岩筒内部构造及其边部构造控制，呈脉状斜列产出。
Silver orebody is controlled by internal and marginal structures of crypto-explosion breccia pipe, and occurs as veins in oblique lines.
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