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作者А·Дмураев等写道,含矿热液上方存在有含汞大气的概念是汞气测量普查方法的基础。对在向斜坳陷中地垒式隆起范围深部断裂结合处的火山成因金矿区进行研究,使用PAФ-I-M型仪器测定汞,灵敏度为1 ×10~(-7)％。分析了10000件样品得知,汞的正常场为:火山岛岩0.63×10~(-0)％,花岗岩类为0.76×10~(-8),疏松沉积物为1.1×10~(-8)％。汞量包围了整个主含矿带,并稍微超过其边界。矿带北部汞量达5.5×10~(-8)％,汞量下查明有金的工业品位。
The author А · Дмураев wrote that the concept of a mercury-containing atmosphere above the mineralized hydrothermal fluids is the basis for the mercury gas measurement survey method. The volcanic gold deposit in the deep fracture junction of the basement uplift in the syncline depression was studied. The mercury content was measured with a PA-I-M instrument with a sensitivity of 1 × 10 -7%. According to the analysis of 10000 samples, the normal mercury field is 0.63 × 10 ~ (-0)% of volcanic island rocks, 0.76 × 10 ~ (-8) for granite and 1.1 × 10 ~ (-8) for loose sediments )%. The amount of mercury encircled the entire main mineralization zone, slightly beyond its borders. The amount of mercury in the northern part of the ore belt reaches 5.5 × 10 -8%, and the industrial grade of gold is ascertained under the amount of mercury.