書誌事項
- タイトル別名
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- Underground Water of the Makimine Mine
- マキホウ コウザン ノ コウナイ ワキミズ ニ ツイテ
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Makimine Mine, Miyazaki Prefecture, works the bedded cupriferous iron sulphidedeposit occured in the black phyllitic formation of the Shimanto Complex. When the underground developments approached the dike of granite porphyry, intruded north of the deposits, the faults bearing the water of high pressure appeared.<BR>These faults are parallel with the dike of granite porphyy, and give little displacement to the deposits, and have the sheared zone of 1 m. in width.<BR>The underground water of these faults has no special chemical component, volume of 4m3/min and pressure of 35-50kg/cm2, and has prevented the underground mine-developments.<BR>For shielding the underground water, cement grouting was effective.
収録刊行物
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- 日本鑛業會誌
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日本鑛業會誌 77 (875), 327-331, 1961
一般社団法人 資源・素材学会
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詳細情報 詳細情報について
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- CRID
- 1390282680957995008
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- NII論文ID
- 40018292903
- 130007254836
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- NII書誌ID
- AN00188932
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- ISSN
- 21856729
- 03694194
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- NDL書誌ID
- 9158240
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- データソース種別
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- JaLC
- NDL
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