| 赛钦铜钴矿成矿地质特征及成因探讨 |
| |
| 引用本文： | 邢高田,范丽琨,王春燕.赛钦铜钴矿成矿地质特征及成因探讨[J].科技信息,2009(9). |
| |
| 作者姓名： | 邢高田 范丽琨 王春燕 |
| |
| 作者单位： | 青海省有色地质矿产勘查院; |
| |
| 摘 要： | 赛钦铜钴矿大地构造位置属秦祁昆地槽褶皱系所属Ⅱ级构造单元—昆仑华力西地槽褶皱带之柴南缘断褶带与东昆仑隆起带的交合部位,昆中深大断裂东段北侧,铜钴矿化赋矿岩性为晚三叠世陆相火山岩建造中的次安山岩。赛钦铜钴矿的形成具有其独特的地质环境和物化条件,而且成矿过程复杂多变,矿床成因与火山—次火山热液有密切的联系,其矿床成因类型为次火山热液型铜钴矿床。
|
| 关 键 词： | 赛钦铜钴矿 次安山岩 矿床成因 次火山热液 |
The Geological Characteristics and Mineralization Condition of Saiqin Cu-Co Deposit |
| |
| XING Gao-tian FAN Li-kun WANG Chun-yan AbastractThe papers aim is to identify practical regional stratigraphic,structural,ma.The Geological Characteristics and Mineralization Condition of Saiqin Cu-Co Deposit[J].Science,2009(9). |
| |
| Authors: | XING Gao-tian FAN Li-kun WANG Chun-yan AbastractThe papers aim is to identify practical regional stratigraphic structural ma |
| |
| Institution: | Geology and Mineral Exploration Institute QingHai provincial Bureau Geology and Mineral;Xining Qinghai;810007 |
| |
| Abstract: | The geostructure position of Saiqin Cu-Co Deposit is located at Qin Qilian-Kunlun to the area located between the respective grade chutes fold belt Chaina East geopolitical fault fold belt mixing up with the shallower parts,the north eastern Kunduz deep faults. Cu-Co Deposit is located in Inferior -Andesite of the land facies volcanic rock construction of the late Sandieshi in time. The formation of Saiqin Cu-Co Deposit has its unique geological environment and the transformation condition. The mineralizati... |
| |
| Keywords: | Saiqin Cu-Co Deposit Inferior-Andesite Ore-deposit origin Inferior volcanic rock hydrothermal |
| 本文献已被 CNKI 等数据库收录！ |
