地球学报Issue(z1)：115-121,7.DOI:10.3975/cagsb.2013.s1.17
都龙锡锌多金属矿床控矿因素及成因的再认识
A Further Discussion on Ore-controlling Factors and Genesis of the Dulong Sn-Zn Polymetallic Deposit in Southeast Yunnan
摘要
Abstract
The Dulong Sn-Zn polymatallic deposit is one of the largest cassiterite sulfide deposits in China. Geological exploration around the Dulong ore district is very important for the continual development of the mining company. Based on the previous exploration and research achievements, this paper discussed ore-controlling factors. It is suggested that this deposit is controlled jointly by Yanshannian granites, the detachment fault system and the Tianpeng Formation. The Yanshanian Laojunshan granites, which seemed to be the most important factor, provided major ore-forming materials and energy; the detachment fault system was favorable for the movement and precipitation of the ore-forming fluid; the Tianpeng Formation offered the profitable physical and chemical conditions for the concentration of ore-forming materials. On such a basis, the authors hold that this deposit should mainly be of magmatic hydrothermal genesis. The ore-prospecting orientations in the area are also pointed out in this paper.关键词
控矿因素/矿床成因/都龙锡锌多金属矿床/滇东南Key words
ore-controlling factors/genesis/Dulong Sn-Zn polymetalic deposit/southeast Yunnan分类
天文与地球科学引用本文复制引用
张世奎,苏航,陶志华..都龙锡锌多金属矿床控矿因素及成因的再认识[J].地球学报,2013,(z1):115-121,7.基金项目
本文由云南华联锌铟股份有限公司科研项目(编号:KY20120910)资助。 （编号:KY20120910）
