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云南大箐锰矿床成矿地质条件综合分析
引用本文:杜发永,杨泽刚.云南大箐锰矿床成矿地质条件综合分析[J].矿产与地质,2006,20(1):19-22.
作者姓名:杜发永  杨泽刚
作者单位:四川省冶金地质勘查院昆明分院,云南,昆明,650224
基金项目:国土资源部国土资源大调查项目
摘    要:通过对该矿区含矿地层特征、矿石物质组分、有关元素含量的综合分析,以及中三叠世该区岩相古地理的研究,说明在中三叠世法郎期,随着海平面的快速上升,来自越北古陆和上地幔的含锰热液中的锰质,在海平面进入相对静止状态时,在半封闭的五凤海湾而聚集成矿。

关 键 词:锰矿床  成矿地质条件  综合分析  云南大箐  五凤海湾
文章编号:1001-5663(2006)01-0019-04
收稿时间:2005-05-01
修稿时间:2005年5月1日

ORE FORMING GEOLOGICAL CONDITION IN THE DAQING MANGANESE DEPOSIT IN YUNNAN
DU Fa-yong,YANG Ze-gang.ORE FORMING GEOLOGICAL CONDITION IN THE DAQING MANGANESE DEPOSIT IN YUNNAN[J].Mineral Resources and Geology,2006,20(1):19-22.
Authors:DU Fa-yong  YANG Ze-gang
Institution:Kunming branch of Sichuan Institute of Metallurgical Geology and Exploration, Kunming , Yunnan , 650224 ,China
Abstract:Based on the comprehensive analysis on the character of the ore bearing strata,ore matter component,related elements in the mine and the research on Middle Cretaceous lithofacies and ancient geography in the area,It is illustrated that during Falang period of Middle Cretaceous epoch,with the rapid rising of the sea level,the manganese matter contained in manganese bearing hydrothermal fluid from North Vietnam old land and upper mantle accumulated to form the deposit on the half closed Wufeng bay when the sea level became relatively static.
Keywords:Manganese deposit  ore forming geological condition  comprehensive analysis  Daqing Yunan  Wufeng bay
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