- 责任者：Chen Xifeng (Institute of Mineral Resources Research ; China Metallurgical Geology Bureau ; Beijing 100025 ; China) ; Peng Runmin
- 刊名：Geology in China
- 出版年：2011
- 卷期：38(5)
- 关键词：构造演化 ; structural evolution ; 成矿控制 ; mineralization controls ; 内蒙古 ; Inner Mongolia
- 页码：p.1201-1211
- 图表：5 illus., 1 table, 30 refs.
- 分类号：1001
- 出版序号：1759
- issnNo：ISSN1000-3657
- isbnNo：CN11-1167/P
Based on an analysis of the geological setting of Langshan area and Aguimiao area, the authors studied the process of geological structural evolution and mineralization. Aguimiao area has experienced a long geological structural evolution and development process, which includes the following stages: 1) the basement rock formation was formed in Neoarchean; 2) the crystalline basement was formed, deformed and metamorphosed in Upper Archean and Lower Proterozoic; 3) the passive continental margin aulacogen was broken up, received sediments and experienced mineralization in Proterozoic; 4) the passive continental margin aulacogen was closed in late Neo-Proterozoic; and 5) the development of compression and orogeny with considerable intrusion of acid-intermediate magma and the deformation occurred from Hercynian to Mesozoic.