| 福建大田狮尾矿区铅锌多金属矿床地质特征与成因初探 |
| |
| 引用本文： | 黄金荣.福建大田狮尾矿区铅锌多金属矿床地质特征与成因初探[J].福建地质,2010,29(3):212-216. |
| |
| 作者姓名： | 黄金荣 |
| |
| 作者单位： | 福建省闽东南地质大队,泉州,362011 |
| |
| 摘 要： | 大田狮尾矿区铅锌多金属矿产于中-下石炭统内,少量产在中-下石炭统与燕山早期二长花岗岩接触带附近。铅锌多金属矿体呈似层状、透镜状展布,矿石组分较复杂,品位中等。为层控-热液改造型铅锌多金属矿床。
|
| 关 键 词： | 铅锌多金属矿 矿床地质特征 大田狮尾 |
Preliminary Study of the Geologic Characteristics and the Genesis of the Shiwei Lead-zinc Polymetallic Deposit in Datian County, Fujian Province |
| |
| Huang Jinrong.Preliminary Study of the Geologic Characteristics and the Genesis of the Shiwei Lead-zinc Polymetallic Deposit in Datian County, Fujian Province[J].Geology of Fujian,2010,29(3):212-216. |
| |
| Authors: | Huang Jinrong |
| |
| Institution: | Huang Jinrong(Southeastern Geology Party of Fujian Province,Quanzhou,362011) |
| |
| Abstract: | The Shiwei lead-zinc polymetallic deposit in Datian County exists in the Middle and Lower Carboniferous strata and some in the contact zone of Middle and Lower Carboniferous strata and Early Yanshanian monzonitic granite.The lead-zinc polymetallic orebody occurs as stratoid or lenticular structures.The component of ore materials is more intricate and the grade of the mineral ores is moderate.It belongs to the lead-zinc polymetallic deposit of the strata-bound hydrothermal reforming type. |
| |
| Keywords: | lead-zinc polymetallic ores geologic characteristics of a mineral deposit Datian County |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
