| 福建宁德禅地铜矿床地质特征及成因初探 |
| |
| 引用本文： | 刘可思.福建宁德禅地铜矿床地质特征及成因初探[J].福建地质,2008,27(4):345-351. |
| |
| 作者姓名： | 刘可思 |
| |
| 作者单位： | 中国地质大学,武汉,430047;福建省第四地质大队,宁德,352100 |
| |
| 摘 要： | 宁德禅地铜矿床产于上侏罗统南园组第三段英安质晶屑凝灰熔岩夹层凝灰岩中。矿体呈脉状、缓倾角似层状，受断裂构造控制，成矿在时空上与中生代中酸性岩浆活动有密切相关，属于岩浆热液交代-充填型铜矿床。
|
| 关 键 词： | 铜矿床 地质特征 成因初探 宁德禅地 |
On Genesis and Geologic Characteristics of the Chandi Copper Deposit in Ningde, Fuj ian Province |
| |
| Liu Kesi.On Genesis and Geologic Characteristics of the Chandi Copper Deposit in Ningde, Fuj ian Province[J].Geology of Fujian,2008,27(4):345-351. |
| |
| Authors: | Liu Kesi |
| |
| Institution: | Liu Kesi (No. 4 Geological Party of Fujian Province, Ningde, 352100) |
| |
| Abstract: | The Chandi copper deposit in Ningde, Fujian Province was discovered in the tuff interlayer of dacite crystal tuff lava of Upper Jurassic Nanyuan Formation. The ore body exists in veins and a parabedded form with a low dip angle, which is controlled by faulted structures. The ore-forming process has a close relation with Mesozoic intermediate and acid magmatic activity in space time. The deposit belongs to the copper deposit of magmatic hydrothermal replacement and filling type. |
| |
| Keywords: | copper deposit geologic characteristics genesis Ningde City Fujian Province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
