- 责任者：Wang Jincao (Guilin University of Technology ; Guilin 541004 ; China) ; Wang Yongdong
- 刊名：Journal of Guilin University of Technology
- 出版年：2012
- 卷期：32(4)
- 关键词：金矿 ; gold ores ; 成矿构造 ; metallotectonics ; 内蒙古 ; Inner Mongolia
- 页码：p.447-454
- 图表：3 illus., 1 table, 13 refs.
- 分类号：1001
- issnNo：ISSN1674-9057
- isbnNo：CN45-1375/N
此刊已审核完Changfulong gold deposit in Inner Mongolia is controlled by a symmetric positive flower joint system. It is suggested that the mineralization zonings of the positive flower joint system are non-ore silicified zone, weak mineralized zone, strong mineralized zone and weak mineralized zone respectively from top to bottom. The strong mineralized zone is located in the “Golden Triangle” area above flower pedicle of the positive flower joint system, namely in the fragmental rock masses encompassed by main joints which dip to the same direction. The mineralization mainly occurred in the metwork fractures and microscopic network fractures with the characteristics of disseminated-veinlet ore-controlling structures as the north-westward reverse strike-slip brittle shear zone. The series of positive flower joint systems are characterized by sinistral echelon and connected by the tensional bridge structures.