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吉尔吉斯南部的汞锑矿床主要与石碳耙的石灰岩、页岩有关.矿床产于石灰岩与页岩的接触带和碳酸盐岩石以及复杂的陆源式喷出岩、页岩岩层中.矿体分为层状的和产于破碎带的交错状两种.位于石灰岩同页岩接触带的层状矿体合矿最富.矿化极不均匀,辰砂呈浸染状、巢状体及被膜状产在碧玉岩角砾岩内,钻探时其岩心采取率极低.1960年前汞锑矿床按一般公认的方法进行了刻槽及岩心取样.岩心样是将岩心沿长轴劈开两半采取的.目前,上述矿床多数已开采,钻孔勘探过的中段业已采掘,个别坑道揭露了过去曾采过样的矿体.由于金属矿物分布极不均匀,有用矿物的品位无
The mercury-antimony deposits in southern Kyrgyzstan are mainly related to the limestone and shale of the rock carbon rakes, which are produced in contact zones and carbonate rocks of limestone and shale, as well as complex terrane-type discharge rocks and shale formations. Layered and produced in the fracture zone staggered two.Lake limestone located in contact with the bedded orebodies is the richest mineralization is extremely uneven, cinnabar was disseminated, nodular and film-like production In jasper breccia, the cores were drilled with extremely low core rates. The mercury-antimony deposits were grooved and core-sampled in a generally accepted manner prior to 1960. Core-like specimens were split between two halves of the core along the long axis , The majority of the above mines have been mined, the middle section of the borehole exploration has been excavated, some of the tunnels exposed the ore bodies that had been mined in the past.Due to the extremely uneven distribution of metal minerals, the grade of useful minerals