| 赵会庆.中国卡林型金矿成矿构造环境及热液特征[J].地质找矿论丛,1999,(3):34-41 |
| 中国卡林型金矿成矿构造环境及热液特征 |
| THE STRUCTURAL BACKGROUND AND CHARACTERISTICS OF ORE-FORMING FLUID OF CARLIN TYPE GOLD DEPOSITS IN CHAIN |
| 投稿时间：1999-06-25 修订日期：1999-08-10 |
| DOI：10.6053/j.issn.1001-1412.1999.3. 005 |
| 中文关键词: 卡林型金矿 构造环境 热液特征 中国 |
| 英文关键词:Carlin type gold deposit structural background characteristics of fluid China |
| 基金项目: |
|
| 摘要点击次数: 1113 |
| 全文下载次数: 2116 |
| 中文摘要: |
| 通过对近年来国内地质界在卡林型金矿研究方面最新成果的对比总结,认为卡林型金矿多产于大地构造活动地带,如不同大地构造单元接合部位,古裂谷带等；成矿物质和成矿热液流体具有多源性,成矿热液为中 弱酸性的低盐度流体,其中含有一定数量的有机质,有机质在成矿过程中起着重要作用。 |
| 英文摘要: |
| According to previous works and data, we can conclude that Carlin type gold deposits in China are mainly located in the tectonically active region, such as the joint of different tectonic elements, ancient rifts etc. Ore-forming materials and hydrothermal fluid of the deposits are multi-sources. The hydrothermal fluid is neutral to weak acid, and contains some organic chemical compounds, which play an important role in the formation of the deposits. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
| 关闭 |
