| 南华大龙潭新近系微细浸染型金矿 |
| |
| 引用本文： | 王锁青,王远航.南华大龙潭新近系微细浸染型金矿[J].云南地质,2004,23(3):328-336. |
| |
| 作者姓名： | 王锁青 王远航 |
| |
| 作者单位： | 云南地矿资源股份有限公司曲靖公司,云南,曲靖,655000 |
| |
| 摘 要： | 大龙潭金矿是云南在新近系砂砾岩中找金新突破。区内矿体分布于NW向断层F4、F6所夹持的大龙潭向斜近核部层间挤压滑动破碎带中,含矿地层为上新统三营组,属微细浸染型。
|
| 关 键 词： | 微细浸染型 金矿 三营组 新近系 大龙潭南华 |
| 文章编号： | 1004-1885(2004)03-328-09 |
THE DALONGTAN NEOGENE MICROSCOPIC DISSEMINATED GOLD DEPOSIT,NANHUA |
| |
| WANG Suo-qing WANG Yuan-hang.THE DALONGTAN NEOGENE MICROSCOPIC DISSEMINATED GOLD DEPOSIT,NANHUA[J].Yunnan Geology,2004,23(3):328-336. |
| |
| Authors: | WANG Suo-qing WANG Yuan-hang |
| |
| Abstract: | The discovery of Dalongtan Au deposit is a new breakthrough of Au prospecting in Neogene Sandstone-Conglomerate of Yunnan. The ore bodies in this area are mainly distributed in the interbed pressed sliding zone nearing the core of Dalongtan syncline between NW-wards fault F_4, F_6. |
| |
| Keywords: | Au Deposit Microscopic Disseminated Type Neogene Dalongtan Nanhua Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
