| 福建安溪铅山铅锌矿床地质特征及成因探讨 |
| |
| 引用本文： | 黄铁民.福建安溪铅山铅锌矿床地质特征及成因探讨[J].福建地质,2008,27(2):186-194. |
| |
| 作者姓名： | 黄铁民 |
| |
| 作者单位： | 福建省闽东南地质大队,泉州,362011 |
| |
| 摘 要： | 铅山铅锌矿位于清流—安溪北西向断裂带与平潭—漳平东西向断裂带的复合部,闽中多金属矿化集中区南端的洛阳—剑斗东西向多金属成矿带中段,矿体贮存于北东向断裂破碎带中,为岩浆期后中低温热液矿床,控矿的北东向断裂带是多期次构造活动的产物,主成矿期为燕山早期,铅山周围尚有较大的找矿远景。
|
| 关 键 词： | 铅锌矿床 地质特征 中低温构造热液型 安溪铅山 |
| 修稿时间： | 2008年3月6日 |
Geologic Characteristics and Genesis of the Qianshan Lead-zinc Deposit in Anxi County of Fujian Province |
| |
| Huang Teiming.Geologic Characteristics and Genesis of the Qianshan Lead-zinc Deposit in Anxi County of Fujian Province[J].Geology of Fujian,2008,27(2):186-194. |
| |
| Authors: | Huang Teiming |
| |
| Institution: | Huang Teiming (Southeastern Geological Party of Fujian Province, Quanzhou, 362011) |
| |
| Abstract: | The Qianshan lead-zinc deposit is situated at the junction part of the Qingliu-Anxi northwest-trend fault zone and the Pingtan-Zhangping east-west-trend fault zone and at the middle section of the Louyang-Jiandou east-west-trend polymetal metallogenetic belt which is located in the southern side of main polymetallic metallization belt in Center Fujian.The ore bodies lay in the northeastern trend fault.It belongs to the mesothermal and epithermal hydrothermal deposit of the magmatic post-stage.The ore-controlled fault zone of the northwestern trend is the product of multi-stage tectonic activities.The main period of mineralization is the early Yanshanian stage.It is considered that there is a great ore-finding perspective around the Qinshan area. |
| |
| Keywords: | lead-zinc deposit geological characteristics mesothermal and epithermal hydrothermal type Anxi County |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
