| 紫金山矿田五子骑龙铜矿床地质特征及成因探讨 |
| |
| 引用本文： | 阮诗昆,龚建生,李文,董艳霞.紫金山矿田五子骑龙铜矿床地质特征及成因探讨[J].有色金属(矿山部分),2009,61(6):37-42. |
| |
| 作者姓名： | 阮诗昆 龚建生 李文 董艳霞 |
| |
| 作者单位： | 紫金矿业集团股份有限公司,福建,上杭,364200 |
| |
| 摘 要： | 通过对五子骑龙铜矿床成矿地质背景、矿床地质特征、矿体特征、成矿地质和物理化学条件等方面的分析,认为本区成矿物质来自燕山晚期岩浆及其后的热液流体,北东向和北西向断裂为主要的控岩控矿和导矿构造,多期次的蚀变分带与成矿密切相关,铜矿(化)体沿构造带向浅部迁移,在裂隙带及两侧沉淀富集成浅成中低温热液脉型硫化铜矿床。
|
| 关 键 词： | 矿床地质特征 矿床成因 浅成中低温热液矿床 五子骑龙 |
Geological Characteristics and Genesis of Wuziqdong Copper Deposits in Zijinshan Area |
| |
| Authors: | RUAN Shikun GONG Jiansheng LI Wen DONG Yanxia |
| |
| Abstract: | Through the analysis of geological environment,geological characteristics,orebody feature,ore-forming geological and physicochemical condition,it is realized that metallogenic material come from magma(late Yanshanian) and hydrothermal water(subsequent Yanshanian).NE and NW faults are main rock-controlling,ore-controlling and ore-transporting structures.Multi-stage alteration zoning has important relation to ore-forming,copper ore(mineralize)body transferred along fault belts to surface and formed Epithermal-Mesothermal sulfide copper deposits. |
| |
| Keywords: | geological characteristics ore genesis Epithermal-Mesothermal deposits Wuziqilong |
| 本文献已被 维普 万方数据 等数据库收录！ |
| 点击此处可从《有色金属(矿山部分)》浏览原始摘要信息 |
|
点击此处可从《有色金属(矿山部分)》下载全文 |
|
