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1983年5月,在伊尔库茨克市苏联科学院西伯利亚分院地壳研究所,召开了全苏《花岗片麻岩穹窿》会议.出席会议的有150多名地质人员,他们来自苏联科学院、苏联地质部及全国各有关高等院校.绝大部分会议报告是研究与花岗片麻岩穹窿及其间坳陷形成有关的成矿作用问题.Ф.А.列特尼科夫强调指出,花岗片麻岩穹窿的形成是白于花岗岩化的发育造成的.В,А.纳尔谢耶夫的报告,从成矿专属性的角度划分出了《穹窿—坳陷》的三种类型.М.З.格卢霍夫斯基等人研究了与古老地合成矿作用有关的大型花岗片麻岩穹窿.М.А.春布拉托夫等人的报告,以南哈萨克斯坦为例,研究了地槽区的花岗岩穹窿的成矿作用问题.А. С.巴雷舍夫阐述了东西伯利亚南部地区穹窿构造对矿床分布的控制作用.
In May 1983, at the Crustal Research Institute of the Siberian Branch of the Soviet Academy of Sciences in Irkutsk, there was a conference called “Granite Gneiss Dome” in the whole Soviet Union. More than 150 geological staff attended the meeting, and they came from the Soviet Academy of Sciences, the Soviet Union Ministry of Geology and the relevant institutions of higher learning throughout the country.Most of the meeting report is to study the granite gneiss domes and the formation of the depression between the formation of the mineralization problems.Lytnikov stressed that the granite The formation of gneiss domes is caused by the development of granite in the middle of the river.Based on the report of Nelson_ev, the report of Nelson_ev made three types of “domes-depressions” from the viewpoint of mineralization specificity.М . G. Glukhovski et al. Studied the large granitic gneiss dome associated with ancient synthetic mineralization. Report by M. A. Brahratov et al. To the south of Kazakhstan, for example, Studied the mineralization of the granite dome in the terrain area .A. Barresev elaborated on the control of the distribution of the dome in the eastern part of Eastern Siberia.