| 冀东长城式金矿赋金角砾状岩石成因初探 |
| |
| 引用本文： | 翟安民.冀东长城式金矿赋金角砾状岩石成因初探[J].地质调查与研究,1998,21(3). |
| |
| 作者姓名： | 翟安民 |
| |
| 作者单位： | 中国地质科学院天津地质矿产研究所!天津，300170 |
| |
| 基金项目： | “九五”地矿部资源与环境科技攻关课题!95－02－003－01，冶金部黄金局冀东金矿课题 |
| |
| 摘 要： | 冀东地区新发现一批产在中元古代碳酸盐岩层中的金矿床（点），文中对该类矿床的容矿围岩特征及其成因、产出的区域构造背景进行了讨论，提出容矿角砾岩是液压致裂角砾岩，是一种矿控构造岩。
|
| 关 键 词： | 长城式金矿 液压致裂作用 矿控构造岩 |
| 修稿时间： | 1998－09－09 |
A PRIMARY DISCUSSION ON THE GENESIS OF ORE-BEARING BRECCIFORM ROCKS OF CHANG CHENG STYLE GOLD DEPOSIT IN EASTERN HEBEI |
| |
| Zhai Anmin.A PRIMARY DISCUSSION ON THE GENESIS OF ORE-BEARING BRECCIFORM ROCKS OF CHANG CHENG STYLE GOLD DEPOSIT IN EASTERN HEBEI[J].Geological Survey and Research,1998,21(3). |
| |
| Authors: | Zhai Anmin |
| |
| Abstract: | A group of gold deposits (points) are newly discovered in the eastern HebeiProvince. The deposits controlled in Middle Proterozoic carhanate rocks-host rocks, belong toChang Cheng style gold deposits. In this paper discussed feature and genesis of host rock, and itoccurrence regional tectonic backgound. At once, suggested that the host breccia is the hydraulicfracturing breccia, is a ore contral structure rock. |
| |
| Keywords: | Chang Cheng style gold deposits hydraulic fracturing ore contral structure rock |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
