论文部分内容阅读
凭经验确定的汞和金在成矿带、矿区、个别矿床范围内,以及在许多矿物中的共生,显然是由于这两种元素具有近似的物理参数和共同的迁移途径与方法造成的。金和汞的成矿作用在空间上的吻合导致形成综合性的金-汞矿床,金-汞矿床是在检查了正在开采或者暂时停产的汞矿床,以及研究较差的汞矿点后才得以发现。综合性矿床特征是含细分散金和具有金汞比值由1:2至1:10的矿体多。根据地质构造位置和成分,综合性金-汞矿床可以分为两组:诺克斯维尔型和卡林型。
Empirically determined mercury and gold in the metallogenic belt, mining area, individual mineral deposits, and in many minerals symbiosis is apparently due to the approximate physical parameters of the two elements and the common migration pathways and methods. The spatial coincidence of the gold and mercury mineralization led to the formation of a synthetic gold-mercury deposit that was obtained after examining the mercury deposits being mined or temporarily decommissioned, as well as the study of poor mercury deposits Find. The comprehensive deposit is characterized by a large number of ore bodies containing finely divided gold and having a ratio of gold to mercury from 1: 2 to 1:10. According to the geological structure of the location and composition of integrated gold - mercury deposits can be divided into two groups: Knoxville and Carlin type.