| 摘要: |
| 层控矿床属火山-沉积变质成因;含铜石英脉型矿床为热液充填成因。根据成矿控制因素和找矿标志,对大宝山地区的成矿远景进行了划分,指出了进一步的找矿方向。 |
| 关键词: 矿床地质特征 矿床类型 找矿方向 大宝山铜矿区 |
| DOI： |
| 附件 |
|
| 基金项目:四川攀西地区铅锌矿资源调查项目;彭县铜矿外围找矿地质调查 |
|
| Geology and exploration prospects of the Dabaoshan copper deposit in Pengzhou,Sichuan |
| MAO Hong-Jiang, LIANG Jing |
(1. No. 606 Party, Sichuan Bureau of Metallurgical Geology and Resources Development, Pengzhou 611930, Sichuan, China;
2. Liwu Copper Industry Co., Ltd., Julong 626201, Sichuan, China) |
| Abstract: |
| Two types of copper deposits are recognized in the Dabaoshan copper mining district in Pengzhou,Sichuan: stratabound and Cu-bearing quartz vein deposits.The stratabound copper deposit should have a volcanic and sedimentary-metamorphic origin while the Cu-bearing quartz vein copper deposit is of hydrothermal filling origin.The delineation of the exploration prospects has been made on the basis of controlling factors and prospecting criteria. |
| Key words: geology deposit type exploration prospect Dabaoshan copper mining district |
