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在苏联吉尔吉斯境内天山地区,查明了许多不同成因类型和工业类型的汞—锑、锡—钨、铋、铅—锌、铜等矿化点。许多研究人员对天山各种类型的内生矿化分布规律在文献中都作了论述。近年来,在解决内生矿化分布规律的问题上进展很大。天山山脉主要由前古生代和古生代岩石组成,而山间盆地被中一新生代和新生代的沉积岩所充填。只有费尔干纳山脉和外阿赖山脉主要由中生代和新生代沉积岩所组成。天山地区内,可以划分为两个最大的独立地质构造单元:乌鲁图一北天山加里东褶皱系和南天山海西褶皱系。北天山褶皱区的加
In the Tianshan Mountains in the Kyrgyz region of the Soviet Union, many mineralization points of mercury-antimony, tin-tungsten, bismuth, lead-zinc, copper and the like have been identified with different genetic types and industrial types. Many researchers have discussed the distribution of various types of endogenous mineralization in the Tianshan Mountains in the literature. In recent years, progress has been made in solving the problem of the distribution of endogenous mineralization. The Tianshan Mountains are mainly composed of Pre-Paleozoic and Paleozoic rocks, while the mountain basins are filled by Cenozoic and Cenozoic sedimentary rocks. Only the Fergana Range and the Exular Range are mainly composed of Mesozoic and Cenozoic sedimentary rocks. Within the Tianshan area, it can be divided into two largest independent geological tectonic units: the Kalurdian fold belt of the Northern Tushan-Ulu Ti-Tainian and the Hercynian fold series of the southern Tianshan. North Tianshan fold area plus