ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
对大洋多金属结核10A锰矿物相的研究
  
关键词:oceanic polymetallic nodules  10A manganese mineral phase
基金项目:
作者单位
刘淑琴 中国地质科学院矿床地质研究所 
潘家华 中国地质科学院矿床地质研究所 
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摘要:
The Research on 10A Manganese Mineral Phase in the Oceanic Polymetallic Nodules
      The conclusion of the research on 10A manganese minerals in the oceanic polymetallic nodules have argued for a long time.In order to explore the species of 10A manganese minerals in our research area,the authors choosed thirteen representative samples mainly composed of 10A manganese minerals from more than 100 nodule samples and studied their thermal stability.Three different cases were summarized:The appearance of 7A diffraction peak and the movement of 10A diffraction peak to higher angle show the existence of buserite Ⅰ and asbolane_buserite mixed_layer mineral in the original samples∶The absence of 7A diffraction peak and the movement of 10A diffraction peak to higher angle indicate that there isn't buserite I but asbolane_buserite mixed_layer mineral in the original samples:The absence of 7A diffraction peak and the basic disappearance of 10A diffraction peak illustrate the existence of asbolane in the original samples;The authors explained above phenomena by using the theory of crystal structure and pointed out that the main species of 10A manganese minerals in the nodules in our research area are buserite Ⅰ,asbolane_buserite mixed_layer mineral and asbolane,no or almost no todorokite is present.
LIU Shu-qin,PAN Jia-hua.1998.The Research on 10A Manganese Mineral Phase in the Oceanic Polymetallic Nodules[J].Acta Geoscientica Sinica,19(3):288-297.
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