Comparison of Internal Structures of Marine Manganese Deposits of Hydrogenetic, Diagenetic and Hydrothermal Origins

Y.Hata; M.Watanabe

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Comparison of Internal Structures of Marine Manganese Deposits of Hydrogenetic, Diagenetic and Hydrothermal Origins

机译：氢成因，成岩作用和热液成因的海洋锰矿床内部结构比较

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Detailed microscopic observation, combined withX-ray diffraction and EPMA analyses of samples from marinemanganese deposits of three different origins, suggests thatcharacteristic internal structures are inherent in each mangansemineral; vernadite (?-MnO2), buserite (10?-manganate) andtodorokite (10?-manganate).

机译：详细的显微镜观察，结合X射线衍射和EPMA对三种不同来源的海相锰矿床样品的分析，表明每个锰矿物具有固有的内部结构。菱铁矿（α-MnO2），堇青石（10β-锰酸盐）和三水铝石（10β-锰酸盐）。

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《Resource Geology 》 |1999年第1期| 共6页
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Y.Hata; M.Watanabe;
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Comparison of Internal Structures of Marine Manganese Deposits of Hydrogenetic, Diagenetic and Hydrothermal Origins

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