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  • 秋田県大葛鉱山の地質と鉱床

    榊原 忠政, 篠原 邦彦 鉱山地質 11 (47), 423-432, 1961

    The Okuzu mine is one of the mines working the beds of the Neogene Tertiary of the Inner Zone of Northeast Japan, and is located immediately to the west of the Osarizawa mine. A thick formation of …

    DOI

  • 秋田県小真木鉱山の地質と鉱床(第2報)

    榊原 忠政 鉱山地質 7 (24), 118-135, 1957

    The prominent feature of the Komaki Mine is the strongly developed supergene enrichment displayed about the Shirane deposit, spreading downward 200-300 meters from the surface of the deposits, and …

    DOI

  • 秋田県小真木鉱山の地質と鉱床(第1報)

    榊原 忠政 鉱山地質 5 (15), 18-32, 1955

    The Komaki mine is one of several mines which is located in the Tertiary mineralized zone of the inner part of north-eastern Japan. It is located immediately to the north of the Osarizawa mine in …

    DOI

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