| 刘腾飞.广西东平表生富集型锰矿床地质特征及成矿条件初步研究[J].地质找矿论丛,1996,(4):42-55 |
| 广西东平表生富集型锰矿床地质特征及成矿条件初步研究 |
| STUDY ON GEOLOGICAL FEATURE AND METALLOGENIC CONDITIONS OF DONPING SUPERGENE ENRICHED Mn ORE DEPOSIT |
| 投稿时间：1996-08-07 修订日期：1996-11-25 |
| DOI：10.6053/j.issn.1001-1412.1996.4. 005 |
| 中文关键词: 东平 氧化锰矿 矿床地质特征 成矿条件 |
| 英文关键词: |
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| 中文摘要: |
| 本文主要论述广西东平表生富集型氧化锰矿床成矿地质环境、含锰岩系地质特征,锰矿层结构,矿石矿物成分及结构构造,矿石化学组分等特征;认为表生富集型氧化锰矿床的形成主要受原生含锰层、地质构造、地形地貌、顶盖层厚度、岩性、气候及水文地质等条件所制约。文章最后讨论了锰矿化富集特征,氧化锰矿成矿模式等并指出探采意义。 |
| 英文摘要: |
| Geological setting, features of the ore bearing rock assemblages, depth, ore structure and texture and mineralogy of Dongping supergene-enriched Mn doposit are discribed in the paper.Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.Based on the mentioned above metallogenic model of the deposit is established. The model can be applied to mining and futher prospecting. |
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