黄金水,汪壁忠,马凤俊.闽西南-粤东锰矿床成因序列、构式和找矿方向[J].地质找矿论丛,1986,(4):1-15
闽西南-粤东锰矿床成因序列、构式和找矿方向
A PRIMARY DISCUSSION ON THE GENETIC PATTERN OF MANGANESE ORE DEPOSITS AND THE EXPLORATION GUIDANCE IN SOUTHEAST FUJIAN EASTERN GUANGDONG DISTRICT
  
DOI:10.6053/j.issn.1001-1412.1986.4. 001
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作者单位
黄金水  
汪壁忠  
马凤俊  
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中文摘要:
      前言闽西南-粤东地区的氧化锰矿,点多面广,其区域分布,与晚古生代、早三迭世的沉积含锰地层关系密切(图1).自五十年代后期开始,闽、粤两省冶金地质队伍就进行找矿勘探工作,地方矿山及群采曾盛极多时.
英文摘要:
      The manganese deposits in southeast Fujian and the eastern Guangdong, which occurred principally in the Variscan and Indo-China fracture depression zone, had undergone the evolution of primary Mn-bearing sedimentary source bed (protore)………………→hydrothermal superimposed Mn ores (or Fe and Mn-bearing polymetallic ores)……………→epithermal and superficial oxidized ores The latter is the main economic concentrations.It is suggested that Mn-bearing source bed, the fracture structure, intrusive contacts and mineral association might be aggregatively regarded as the guidance for prospecting
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