而成矿体系中碲金银矿、碲银矿等低温同质多像变体的存在，反映了该类型矿床形成于成矿温度和压力较低的环境条件下。
The existence of petzite and hessite as low-temperature isomorphic modifications indicates that this kind of deposits has been formed in the low temperature and low pressure environment.
而成矿体系中碲金银矿、碲银矿等低温同质多像变体的存在，反映了该类型矿床形成于成矿温度和压力较低的环境条件下。
The existence of petzite and hessite as low-temperature isomorphic modifications indicates that this kind of deposits has been formed in the low temperature and low pressure environment.
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