The New Knowledge of Metallogenetic Rules and Ore-Controlling Factors of Heqing Mn Deposit, Yunnan Province
详细信息
- 责任者：Wei Ronghua (Nonferrous Geological Team 310 of Yunnan ; Dali 671000 ; China) ; Yang Zhibin
- 刊名：Yunnan Geology
- 出版年：2009
- 卷期：28(4)
- 关键词：锰矿 ; manganese ores ; 云南 ; Yunnan Province
- 页码：p.415-419
- 图表：1 illus., 7 refs.
- 分类号：1001
- issnNo：ISSN1004-1885
- isbnNo：CN53-1041/P
摘要
The Heqing Mn deposit exists in the Indosinian EW fault depression. The metallogenetic time must be earlier than the middle—late Beiya stage of Songgui period, which can be divided into the cogenetic sedimentation type and the leaching filling type. The ore-controlling structure is the special “sag of pot bottom” of synclinal axis. The genesis belongs to the volcanic hydrothermal cogenetic sedimentation and posterior reformation type Mn deposit.
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