| 孙树浩.内蒙古宁城地区煌斑岩与金矿[J].地质找矿论丛,1997,(1):59-66 |
| 内蒙古宁城地区煌斑岩与金矿 |
| LAMPROPHYRES AND GOLD DEPOSIT IN NINGCHENG AREA, INNER MONGOLIA |
| 投稿时间：1996-12-16 修订日期：1997-01-28 |
| DOI：10.6053/j.issn.1001-1412.1997.1. 008 |
| 中文关键词: 煌斑岩脉 韧性剪切带 热液型金矿 |
| 英文关键词:Lamprophyre vein ductile shear zone hydrothermal gold deposit |
| 基金项目: |
|
| 摘要点击次数: 1253 |
| 全文下载次数: 1706 |
| 中文摘要: |
| 内蒙古宁城地区出露加里东海西期煌斑岩脉群,其中云斜煌斑岩内,沿燕山期韧性剪切片理化带,分布金矿体。煌斑岩是宏观找金的标志。金矿体中硅化、绿泥石化、方解石化发育。主要金属矿物是黄铁矿。金主要以显微和次显微自然金包裹体,赋存于黄铁矿内。微量元素V、Ni浓度高。与金相关的元素为Bi、Mo,金矿成因类型为幔源C－H－O流体分异演化热液型金矿。 |
| 英文摘要: |
| In Ningcheng Area, Inner Mongolia Au ore bodies Occur along schistozed rock zone of the Yanshenian ductile shaar zone within lamprophyres, which are Au ore prospecting target macro scopicaly. The ore bodies are developed with silicification, chloritization and calcitization. Pyrite is the major ore mineral. Micro and sub-micro native gold inclusion is the dominant occurrence in pyrite. Micro-elements of V and Ni are in higher concentration and Bi, Mo are correlated to Au.The Au deposit is of mentle-sourced C-H-O differentiational and evolutional hydrothermal fluidGold deposit. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
| 关闭 |
