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库兹涅茨克一阿尔泰汞矿带是阿尔泰一萨彦褶皱区西部最重要的控矿构造,该褶皱区作为独立汞矿省是中亚次大陆中生代构造-岩浆活动带和汞矿化带的一个组成部分。近年来的研究提供的大量事实表明,中生代构造-岩浆活动带阶段,无论对该矿带地质构造的形成或其一定的成矿专属性——主要发育汞矿石建造的低温热液汞矿床,都起着非常重要作用。然而,对于这些矿床形成的时代和成因还存在着另外一些认
The Kuznetsk-Altay mercury deposit is the most important ore-controlling structure in the west of the Altay-Sayan fold zone, which is an independent mercury mine and one of the Meso-Central Subcontinent tectono-magmatic activity zones and mercury mineralization zones component. The large number of facts provided by recent studies suggest that both the Mesozoic tectono-magmatic activity stage, both for the formation of the ore belt or its metallogenic specificity, is dominated by low-temperature hydrothermal mercury deposits constructed of mercury ore Plays a very important role. However, there are other acknowledgments about the age and causes of the formation of these deposits