| 广东省藤铁铁矿成矿地质特征 |
| |
| 引用本文： | 武金阳. 广东省藤铁铁矿成矿地质特征[J]. 地质找矿论丛, 2005, 20(Z1): 131-133 |
| |
| 作者姓名： | 武金阳 |
| |
| 作者单位： | 中国冶金地质勘查工程总局,第二地质勘查院,福建,莆田,351111 |
| |
| 摘 要： | 藤铁铁矿位于鱼鹿岩枝东接触带中段,该矿体为铁、铜、锡共(伴)生矿床.受断裂带、岩体侵入接触带、夕卡岩带和鱼鹿岩枝控制.据此总结出该区"三带一体"的成矿特征.
|
| 关 键 词： | 藤铁、铁铜共(伴)生矿 鱼鹿岩枝 " 三带一体" 广东省 |
| 文章编号： | 1001-1412(2005)S0-0131-03 |
| 修稿时间： | 2005-03-21 |
GEOLOGICAL FEATURE OF TENGTIE Fe DEPOSIT IN GUANGDONG PROVINCE |
| |
| WU Jin-yang. GEOLOGICAL FEATURE OF TENGTIE Fe DEPOSIT IN GUANGDONG PROVINCE[J]. Contributions to Geology and Mineral Resources Research, 2005, 20(Z1): 131-133 |
| |
| Authors: | WU Jin-yang |
| |
| Abstract: | Tengtie Fe deposit is acompanied by Cu and Sn located at the middle part of the east contact zone of Yulu apophyse. It is controlled by fracture contact zone, skarn zone and the apophyse. |
| |
| Keywords: | Tengtie by-product of Cu and Sn Yulu apophyse fracture zone-contact zone skarn zone-apophyse control Guangdong province |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
