| 福建建阳大金山铅锌矿床地球物理化学异常特征 |
| |
| 引用本文： | 何道金.福建建阳大金山铅锌矿床地球物理化学异常特征[J].福建地质,2008,27(4):377-384. |
| |
| 作者姓名： | 何道金 |
| |
| 作者单位： | 福建省地质调查研究院,福州,350011 |
| |
| 摘 要： | 大金山铅锌矿位于泰宁一政和北东东向铜多金属成矿带上，是该成矿带主要的矿种之一，也是闽北地区一个较有价值的矿床。矿床产于早元古代南山组上段，受燕山期北东东向构造控制，属中低温热液充填交代型矿床。
|
| 关 键 词： | 铅锌矿床 地球物理 地球化学 异常 建阳大金山 |
Geophysical and Geochemical Anomaly Characteristics of Dajinshan Lead-zinc Deposit in Jianyang County, Fujian Province |
| |
| He Daojin.Geophysical and Geochemical Anomaly Characteristics of Dajinshan Lead-zinc Deposit in Jianyang County, Fujian Province[J].Geology of Fujian,2008,27(4):377-384. |
| |
| Authors: | He Daojin |
| |
| Affiliation: | He Daojin (Fujian Institute of Geology Survey and Research, Fuzhou, 350011) |
| |
| Abstract: | The Dajinshan Lead-zinc Deposit, situated at the copper polymetal metallogenetic belt of Taining-Zhenghe north-east-east trend, is one of valuable mineral deposits in Northern Fujian.It exists in the upper segment of Early Proterozoic Nanshan Formation strata and is controlled by the north-east-east structures of Yanshanian Stage. The deposit belongs to the ones of the intermediate and low temperature hydrothermal filling and metasomatic type. |
| |
| Keywords: | lead-zinc deposit geophysics geochemistry anomaly Jianyan County |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
