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铊(T1)是自然界很稀少的分散元素。铊矿物在自然界中极其稀少,1984年前已知的铊矿物不过10个。1977年,斜硫砷汞铊矿(Christite)为A·Radfke等人第一次在美国内华达州卡林型金矿中发现,我省这次的发现仅是自然界中第二次的发现.有关研究指出,铊矿物仅形成于热液作用的低温阶段,多数是硫化物和含硫盐类,个别是硒化物和氧化物。我省是在低温热液汞矿床中发现,为硫盐矿物,但不是文献中所指形成于岩浆期后热液矿床,而是在沉积再造矿床中。该矿物发现于贵州兴仁滥木厂汞矿床中.
Thallium (T1) is a very rare scattered element in nature. Thallium minerals are extremely rare in nature, but there are only 10 thallium minerals known until 1984. In 1977, for the first time, A. Radfke et al. Were found in Carlin-type gold deposits in Nevada, USA, and the discovery of this province was only the second discovery in nature. The study indicates that thallium minerals are only formed in the low temperature stage of hydrothermal reaction, most of them are sulfides and sulfur salts, and selenides and oxides are individual. The province is found in low-temperature hydrothermal mercury deposits as sulfur salts, but not in the literature as formed in the magmatic post-hydrothermal deposits, but in the sedimentary re-deposit. The mineral was found in the mercury deposit at Xingren Industrail Factory in Guizhou Province.