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业已查明,全球范围内的汞矿化基本上分布在三个汞矿带:地中海汞矿带,太平洋汞矿带和中亚汞矿带。前两个汞矿带位于阿尔卑斯期和中生代的褶皱区,而第三个汞矿带的形成则与中亚褶皱带古生代构造的中生代构造-岩浆活化作用有关。 据(1946)计算,全部汞矿床中的含汞量仅占地壳总汞量的0.02％左右。近20年来对金属矿床和石油天然气矿床中含汞量的广泛研究结果表明,在这些地质体中富集有可观数量的汞,虽然它们的总含汞量未必能从根本上改变的计算结果。在大多数情况下这些汞都可顺便回收,而
It has been identified that mercury mineralization is distributed globally across three mercury zones: the Mediterranean Mercury Zone, the Pacific Mercury Zone and the Central Asia Mercury Zone. The first two mercury zones are located in the alpine and Mesozoic fold zones, whereas the third zone is associated with the Mesozoic tectono-magmatic activation of the Paleozoic fold in the Central Asia fold zone. According to (1946), the mercury content of all mercury deposits only accounts for about 0.02% of the total mercury in the crust. Extensive research into the mercury content of metal deposits and oil and gas deposits in the past two decades has shown that considerable amounts of mercury are enriched in these geologies, although their total mercury content may not be able to change fundamentally. In most cases, these mercury can be recovered by the way, and