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- 石原 舜三
- Geological Survey of Japan
書誌事項
- タイトル別名
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- The magnetite-series and ilmenite-series granitic rocks.
- 磁鉄鉱系花崗岩類とチタン鉄鉱系花崗岩類〔英文〕
- ジテッコウケイ カコウガンルイ ト チタン テッコウケイ カコウガンルイ エイ
この論文をさがす
抄録
Opaque minerals of common granitic rocks were studied microscopically. The granitoids were divided into (i) a magnetite-bearing magnetite-series and (ii) a magnetite-free ilmenite-series. Each series has the following characteristic assemblages of accessary minerals:<BR>Magnetite-series: Magnetite (0.1-2 vol.%), ilmenite, hematite, pyrite, sphene, epidote, high ferric/ferrous (and high Mg/Fe) biotite;<BR>Ilmenite-series: Ilmenite (less than 0.1 vol.%), pyrrhotite, graphite, muscovite, low ferric/ferrous (and low Mg/Fe) biotite.<BR>The mineral assemblages imply a higher oxygen fugacity in the magnetite-series granitoids than in the ilmenite-series granitoids during solidification of the granitic magmas. The boundary separating the two series is probably near the Ni-NiO buffer.<BR>The magnetite-series granitoids are considered to have been generated in a deep level (upper mantle and lowest crust) and not to have interacted with C-bearing materials; whereas the ilmenite-series granitoids were generated in the middle to lower continental crust and mixed with C-bearing metamorphic and sedimentary rocks at various stages in their igneous history. The former carries porphyry copper-molybdenum deposits and the latter accompanies greisen-type tin-wolframite deposits. Lack of porphyry copper deposits in the Mesozoic orogeny belts in East Asia is related to a general paucity of the magnetite-series granitoids in this terrane.
収録刊行物
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- 鉱山地質
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鉱山地質 27 (145), 293-305, 1977
資源地質学会
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キーワード
詳細情報
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- CRID
- 1390001206526161024
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- NII論文ID
- 130003639441
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- NII書誌ID
- AN00082385
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- COI
- 1:CAS:528:DyaE1cXhsleqs78%3D
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- NDL書誌ID
- 1848053
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- ISSN
- 00265209
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
- CiNii Articles
- Crossref
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- 抄録ライセンスフラグ
- 使用不可