<報文>秋田県白岩鉱山のマンガン鉱床 : とくに水マンガン鉱のγ型ラムスデル鉱化について

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  • アキタケン ハクガン コウザン ノ マンガン コウショウ トクニ スイマンガンコウ ノ ガンマガタ ラムスデルコウカ ニ ツイテ
  • <Original Papers>Manganese Ore Deposits of Shiraiwa Mine, Akita Prefecture : With Special Reference to the Alteration of Manganite to γ-type Ramsdellite by Weathering

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The bedded manganese ore deposits of Shiraiwa Mine occur in andesitic breccia tuff of miocene age. The hypogene manganese minerals in the deposits mainly consist of pyrolusite and manganite with a small quantity of rhodochrosite. In the upper zones of the deposits, γ-type ramsdellite and part of pyrolusite are formed by the weathering of manganite. The alteration process of the mineral may be summarized as follows : [figure] The existence of two alteration processes of manganite is due to the difference in oxidation environments.

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