| 云南中甸松诺铜多金属矿床成矿特征 |
| |
| 引用本文： | 吴俊,董涛.云南中甸松诺铜多金属矿床成矿特征[J].云南地质,2013(4):409-411. |
| |
| 作者姓名： | 吴俊 董涛 |
| |
| 作者单位： | 云南省地质调查院矿产所,云南昆明650216 |
| |
| 摘 要： | 松诺铜多金属矿区地质背景类似于普朗铜矿,异常元素组合与普朗斑岩型铜矿相似,同时均属同一构造岩浆岩带,松诺是寻找“普朗式铜矿”最有利地段.
|
| 关 键 词： | 三类铜多金属矿 印支期斑岩控矿 三叠系地层赋矿 格咱成矿带中部 云南中甸松诺 |
THE METALLOGENESIS FEATURE OF SONGNUO CU MULTIMETALLIC OREFIELD IN ZHONGDIAN,YUNNAN |
| |
| WU Jun,DONG Tao.THE METALLOGENESIS FEATURE OF SONGNUO CU MULTIMETALLIC OREFIELD IN ZHONGDIAN,YUNNAN[J].Yunnan Geology,2013(4):409-411. |
| |
| Authors: | WU Jun DONG Tao |
| |
| Institution: | (Branch of Mineral Resources, Yunnan Institute of Geological Survey, Kunming 650216) |
| |
| Abstract: | The geological setting of Songnuo Cu muhimetallic orefield is similar to that of the Pulang Cu de- posit. The element assemblage of anomaly is similar to that of Pulang porphyry Cu deposit, belonging to the same structure magmatic rock zone. Songnuo area is the most advantageous one in the search for ＂Pulang type Cu depos-it＂. |
| |
| Keywords: | Triassic Intermediate -Acid Rock Body Geochemical Feature Pulang Type Cu Deposit |
| 本文献已被 维普 等数据库收录！ |
