| 铜山铜矿矿床地质特征及找矿方向探讨 |
| |
| 引用本文： | 俞沧海. 铜山铜矿矿床地质特征及找矿方向探讨[J]. 中国矿山工程, 2002, 31(3): 1-3 |
| |
| 作者姓名： | 俞沧海 |
| |
| 作者单位： | 铜陵有色金属(集团)公司,安徽,铜陵,244001 |
| |
| 摘 要： | 铜山铜矿床控矿因素有地层、岩浆岩、构造 ,层间断裂及接触带是主要容矿构造 ,矿床成因为层控矽卡岩型铜矿床。矿体空间上的分布规律表现为“尖灭再现”或“尖灭侧现”的特点 ,“铜山下部找前山”、“前山深部找前山”是铜山地区的重要找矿方向 ,铜山地区东南部具有找矿前景
|
| 关 键 词： | 铜矿床 控矿因素 空间分布规律 找矿方向 |
| 文章编号： | 1002-8951(2002)03-0001-03 |
| 修稿时间： | 2001-06-07 |
Geological characters and prospecting direction of Tongshan copper deposit |
| |
| YU Cang hai. Geological characters and prospecting direction of Tongshan copper deposit[J]. China Mine Engineering, 2002, 31(3): 1-3 |
| |
| Authors: | YU Cang hai |
| |
| Abstract: | Ore control factors are strate, magmatic rock and structure in Tongshan copper deposit. Interlayer faults and contact zone are main including ore structures. The genetic type of deposit is strata bound skarn type copper deposit. The regularity of spatial distribution of orebodies is reappearing or appearing at flank after disappearing. It is main prospecting direction that finding copper orebodies of Qianshan type under Tongshan and depth of Qianshan. There is prospecting foreground at southeast of Tongshan area. |
| |
| Keywords: | copper deposit ore control factor regularity of spatial distribution prospecting direction |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
