Metallogenetic Characteristics of Multi-Metal Belt at Triassic Aulacogen Margin in oft-com:office:smarttags" />South Qinling
详细信息
- 责任者：Zhang Hongbin (Geological Survey of Gansu Province ; Lanzhou 730000 ; China) ; Wang Chaijin
- 刊名：Gansu Geology
- 出版年：2011
- 卷期：20(3)
- 关键词：多金属矿 ; polymetallic ores ; 断裂带 ; fracture zones ; 秦岭 ; Qinling Mountains
- 页码：p.60-65
- 图表：3 illus., 1 table, 5 refs.
- 分类号：1001
- 出版序号：554
- issnNo：ISSN1004-4116
- isbnNo：CN 62-1191/P
摘要
Triassic aulacogen in South Qinling is located between Hezuo-Tanchang-Liangdang fault and Lazikou-Zhouqu-Chengxian fault, extending eastward into Shanxi Province, westward into Qinhan Province. Traditionally, the northern margin of this fault zone is deemed as the boundary between Middle Qinling and South Qingling, along which a lot of multi-metal ore occurrences and mineralized points were discovered. The evidences of some multi-metal deposits support that the deposits in the tectonic belt mainly are fallen into metallogenetic type of brine water.oft-com:office:office" />