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本文通过多种分析手段，论证了深海结核中钡镁锰矿的存在和它的矿物学特征及其与主要金属元素间的关系，探讨了影响钡镁锰矿分布的主要因素。是：与当地的地化环境有关，氧化还原电位的高低直接影响着钡镁锰矿的形成；Ｅｈ值低的环境有利于它的生成；阳离子（如Ｍｎ２＋、Ｎｉ２＋、Ｃｕ２＋、Ｚｎ２＋等）的类质同象又往往造成Ｍｎ和这些元素成正相关；弱氧化还原环境并呈半流动态的沉积物液化层有利于Ｍｎ２＋迁移，又是Ｍｎ聚集的地方，它为钡镁锰矿生成的理想层位；后期重结晶作用，又导致部分非晶质转化成钡镁锰矿；超微生物对深海锰结核──锰质核形石乃至钡镁锰矿的生成起着建造者的作用。认为：在选矿冶炼时，以选择表面粗糙或半粗糙型结核为最佳矿样。
This paper demonstrates the existence of the barium mafic manganese ore and its mineralogical characteristics in deep sea nodules and its relationship with the major metal elements by a variety of analytical methods. The main factors affecting the distribution of barrenite ore are discussed. Is: It is related to the local geochemical environment. The redox potential directly affects the formation of barium magnesiite. The low Eh environment is favorable for its formation. The cations (such as Mn2 +, Ni2 +, Cu2 +, Zn2 +, etc.) Isomorphism also tends to cause a positive correlation between Mn and these elements; weakly redox environment and was semi-fluid sediment liquefaction layer is conducive to Mn2 + migration, but also the place where Mn is aggregated, which is ideal for the formation of barium manganese ore; late Recrystallization, but also led to the conversion of some amorphous into barium magnesium manganese ore; supermicroorganisms on the deep-sea manganese nodules ─ ─ manganese-type nuclei or even barium manganese ore generation play a role as a builder. That: the dressing smelting, to choose the rough surface or semi-rough tuberculosis as the best ore samples.