• 责任者：Wang Lei (Faculty of Land and Resource Engineering ; Kunming University of Science and Technology ; South-West Institute of Geological Survey ; Geological Survey Center for Nonferrous Metals Resources ; Kunming 650093 ; China) ; Han Runsheng
• 刊名：Geological Bulletin of China
• 出版年：2011
• 卷期：30(4)
• 关键词：铜矿 ; copper ores ; 成矿规律 ; metallogenic regularity ; 云南 ; Yunnan Province
• 页码：p.605-611
• 图表：6 illus., 1 table, 13 refs.
• 分类号：1001
• issnNo：ISSN1671-2552
• isbnNo：CN11-4648/P

Yimen Fengshan copper deposit is a typical example of Yimen-type copper deposit which is located in the copper mineralized zone of Kunyang rift valley, Yunnan Province, China. The deposit is evidently controlled by diapir and structure, and ore bodies are located in cataclastic dolomite of Lüzhijiang Formation Fengshan member. Diapir structure is a special structural feature with the old tectonic massif pierced in the new formation. By researching Fengshan ore bodies, diapir of controlling ore bodies and construction features, the authors discovered that diapir and constructs have the tendency of W-SW, and diapir has the feature of S-SW side of V. By controlling of the two features, ore bodies with the S-SW side of the V characteristics, the characteristics provide an important basis for the formation mechanism of diaper and the deep ore-finding prognosis.