碲金银矿

The contents of gold in hessite and petzite vary largely from trace to 26.1wt%, which is believedto occur as an isomorphic formof Ag in hessite.

金在金-银碲化物中的含量随温度降低而升高，相关矿物的形成顺序为碲银矿-碲金银矿-。

The major telluride minerals are hessite and petzite, with some alaite and tellurobismuthite intergrowthed, occurring as a closely paragenetic group in inter-crystal porosesor fractures of sulfides and gangue minerals.

碲银矿和碲金银矿中Au含量变化较大，w为痕量至26.1%，与银呈负相关，与铋为正相关，可能是以类质同象形式替代Ag进入到碲银矿中；碲铅矿中未检测到金。

From mineral associations ofnative gold -calaverite, ga1ena -altaite in conunon, and native silver-hessite at the endof the sulfides quartz stage, it is concluded that Te, fugacity is in "unstheated statefor native Te" and will decline with the temperature of metallogeulc fluids decreased.

自然金-跨金矿、碲铅矿-方铅矿与晚阶段碲银矿-自然银共生组合分析表明，本区碲逸度处于&自然碲的不饱和&状态，并随成矿温度降低而减小。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。