| 吉林二道甸子金矿床的地质特征及其成因 |
| |
| 引用本文： | 吴尚全,张文起.吉林二道甸子金矿床的地质特征及其成因[J].黄金,1993,14(1):1-6. |
| |
| 作者姓名： | 吴尚全 张文起 |
| |
| 作者单位： | 吉林有色地质勘查局研究所
(吴尚全，张文起，刘松义)，吉林有色地质勘查局研究所(杨翼) |
| |
| 摘 要： |
|
| 关 键 词： | 地质特征 复成矿床 金矿 |
Geological characters and genesis of Er-Dao-Dian-Zi Gold Deposit, Jilin Province |
| |
| Wu Shangquan et al..Geological characters and genesis of Er-Dao-Dian-Zi Gold Deposit, Jilin Province[J].Gold,1993,14(1):1-6. |
| |
| Authors: | Wu Shangquan |
| |
| Affiliation: | Jilin Institute of the Bureau of Geological Exploration of Non-Ferrous Metals |
| |
| Abstract: | The geological characters of Er-dao-Dian-Zi Gold Deposits are as follows:
1) The forms of the ore body is under the control both fault strutures and in-terbedding horizons of biotite-quartz hornberg and plagioclase-hornblende hornberg.
2) Deuterogenic auriferous quartz-veins and contemporagenic lamellar sulfides associatively occur. 3) There are two mineralization stages of meso and low-temperature. 4) Compositions of the fluid inclusion displayed some features of strabound or magmatic hydrothermal deposits. Therefore, this deposits belongs to polygenetic magma-hydrothermal one. |
| |
| Keywords: | geological characters polygenetic deposits |
| 本文献已被 CNKI 维普 等数据库收录！ |
