| 王宝德,牛树银,孙爱群,刘亚明,郭鹏志,孙双海.冀北万全寺银金矿床地质地球化学特征[J].地质与勘探,2008,(1):15-20 |
| 冀北万全寺银金矿床地质地球化学特征 |
| GEOLOGY AND GEOCHEMISTRY OF WANQUANSI SILVER-GOLD DEPOSIT,NORTH HEBEI PROVINCE |
| 投稿时间：2006-12-18 修订日期：2007-03-09 |
| DOI： |
| 中文关键词: 万全寺银金矿床 地质地球化学特征 冀北 |
| 英文关键词: Wanquansi Ag- Au deposit, geology and geochemistry, north Hebei |
| 基金项目:河北省科研项目 |
| 王宝德 牛树银 孙爱群 刘亚明 郭鹏志 孙双海 |
| [1]石家庄经济学院地质调查研究院,石家庄050031 [2]天津华北地质勘查总院,天津300181 |
| 摘要点击次数: 2174 |
| 全文下载次数: 1800 |
| 中文摘要: |
| 万全寺银金矿床位于张宣幔枝构造东侧的侏罗纪断陷盆地中,成矿时限晚于133.33Ma～101.82 Ma.通过硫、铅、氢、氧、碳及稀有气体同位素研究认为,成矿物质应源自地球深部,在中生代冀西北幔枝构造演化过程中集中成矿.成矿热液以岩浆水为主并加入了部分天水. |
| 英文摘要: |
| Wanquansi Ag- Au deposit is located in the Jurassic fault depression at the east part of Zhangiiakou -Xuanhua mantle branch structure. Ag- Au mineralization is posterior to 101.82 to 133.33 Ma. Based on sulfur, lead, oxygen, carbon and noble gases isotopes, it is considered that the mineralizing materials came from the deep mantle. Economic ores were concentrated in the process of mantle branch evolution during Mesozoic. Hydrotherreal fluids were dominated by magmatic water with some meteoric water. |
|
查看全文
查看/发表评论 下载PDF阅读器 |
| 关闭 |
|
|
|
