| 吉林省龙井市后底洞金矿床地质特征及找矿思路 |
| |
| 引用本文： | 时俊峰,朴景道,钟瑞绩.吉林省龙井市后底洞金矿床地质特征及找矿思路[J].吉林地质,2001,20(3):18-22. |
| |
| 作者姓名： | 时俊峰 朴景道 钟瑞绩 |
| |
| 作者单位： | 吉林有色地勘局603队,吉林,珲春,133300 |
| |
| 摘 要： | 后底洞金矿床产于二叠纪柯岛组变质岩系与华力西期辉长岩体内外接触带。矿化类型为含金蚀变岩型，矿体受北东向断裂构造控制，矿床成因类型为次火山热液型。
|
| 关 键 词： | 金矿床 地质特征 找矿思路 吉林 金矿化 断裂构造 |
| 文章编号： | 1001-2427(2001)03-0018-05 |
The geological features of the Houdidong Au deposit, Longjing, Jilin province and its train of thought for ore prospecting |
| |
| SHI Junfeng,PIAO Jingdao,ZHONG Ruiji.The geological features of the Houdidong Au deposit, Longjing, Jilin province and its train of thought for ore prospecting[J].Jilin Geology,2001,20(3):18-22. |
| |
| Authors: | SHI Junfeng PIAO Jingdao ZHONG Ruiji |
| |
| Abstract: | The Houdidong Au deposit occurred in the Permian, Kedao Formation contact zone between metamorphic rock series and Variscan gabbro body. The mineralized type belongs to gold-bearing altered rock one, ore body is controlled by faulted structure with NE strike. The genetic type of deposit is subvolcanic hydrothermal one. |
| |
| Keywords: | Au deposit geologic features the train of thought for prospecting Houdidong |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
