| 于都县银坑矿田F1断裂特征及其控矿作用 |
| |
| 引用本文： | 高贵荣,林长仔.于都县银坑矿田F1断裂特征及其控矿作用[J].江西地质,2000,14(1):49-53. |
| |
| 作者姓名： | 高贵荣 林长仔 |
| |
| 作者单位： | 江西省地质矿产勘查开发局赣南地质调查大队!江西赣州341000 |
| |
| 摘 要： | 于都县银坑矿田的Ｆ１断裂是该矿田区域性推覆前峰，其断裂规模大，活动时间较长，在银坑矿田控制了地层、岩浆岩和多金属矿化的展布。本文主要从断裂的形象特征入手，浅析了断裂的控矿作用，同时指出Ｆ１断裂不但具有导岩导矿意义，耐用还有储矿作用。断裂本身亦具有重要的找矿意义。
|
| 关 键 词： | 断裂特征 控矿作用 于都县 银坑矿田 银矿床 |
CHARACTERISTICS OF F_1 FAULT IN THE YINKENG OREFIELD OF YUDU COUNTY AND ITS ORE-CONTROLLING ROLE |
| |
| GAO Gui-rong,LIN Chang-zi.CHARACTERISTICS OF F_1 FAULT IN THE YINKENG OREFIELD OF YUDU COUNTY AND ITS ORE-CONTROLLING ROLE[J].Jiangxi Geology,2000,14(1):49-53. |
| |
| Authors: | GAO Gui-rong LIN Chang-zi |
| |
| Abstract: | As a regional nappe front in the Yinkeng orefield of Yudu County, F_1 is a large scale fault with a long activity history that controls the distribution of strata, igneous rocks and metallization in the Yinkeng orefield. starting with its apparent features, this paper explains its role in controlling ores and points out further that it was not only a passageway for magma and ore fluids, but also a structure for ore accommodation. The fault itself has an important significance in ore search. |
| |
| Keywords: | fault characteristics role in controlling ores Yinkeng Yudu county Jiangxi |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
