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在前人研究成果及国内、外已有大量地质、矿产资料的基础上,通过对亚洲东部区域地质构造及矿产资料的综合分析,本文试图对该地区有色金属成矿域的划分,成矿及分布特征等进行一些初步探讨。文中所指亚洲东部包括维尔霍扬-楚科奇褶皱区,蒙古-鄂霍次克褶皱系东段,内蒙古-兴安褶皱区,锡霍特褶皱系,中朝地台,秦岭褶皱系东段,扬子地台,华南褶皱系,缅马褶皱系,印支褶皱系等及亚洲所属诸岛屿。涉及的有色金属矿床有铜、铅锌、钨、锡、钼、锑、汞、金等。根据区域地质构造,区域矿床分布及成矿特征,将亚洲东部自东而西分为岛弧成矿域,大陆边缘成矿域及大陆区成矿域(图1)。
Based on the research results of predecessors and a large number of geological and mineral resources both at home and abroad, this paper attempts to analyze the geologic structure and mineral resources in east Asia and analyze the classification of ore-forming areas, Distribution characteristics such as some preliminary discussions. The eastern Asian part of this paper includes the Verhoe-Chukotka fold zone, the Mongolia-Okhotsk fold series, the Inner Mongolia-Xing’an fold zone, the Sikhot fold series, the Sino-Korean platform, the eastern Qinling fold series, Yangtze platform, South China folds, Myanmar Burma folds, Indosinian folds and other Asian-owned islands. Non-ferrous metal deposits involved in copper, lead and zinc, tungsten, tin, molybdenum, antimony, mercury, gold and so on. According to regional geological structure, regional ore deposits and metallogenic characteristics, the east of East Asia is divided into island arc mineralization, continental margin mineralization and continental region (Figure 1).