西オーストラリア・ハマースレイ地域の縞状鉄鉱床中に胚胎する高品位鉄鉱床の下盤頁岩の熱水変質について--全岩化学組成,同位体組成,流体包有物による検討
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概要
- 論文の詳細を見る
- Society of Resource Geologyの論文
- 2003-06-15
著者
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春名 誠
Department Of Geosciences The Pennsylvania State University
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Ohmoto Hiroshi
Department Of Veterinary Public Health Faculty Of Veterinary Medicine Hokkaido University
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Ohmoto Hiroshi
Department Of Geosciences The Pennsylvania State University
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Fujimaki Hirokazu
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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Fujimaki Hirokazu
Institute Of Mineralogy Petrology And Econimic Geology Faculty Of Science Tohoku University
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Haruna Makoto
Department Of Geosciences The Pennsylvania State University
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HANAMURO Takahiro
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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UYEDA Kaoru
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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Uyeda Kaoru
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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Hanamuro Takahiro
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
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花室 孝弘
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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上田 薫
Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University
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- 西オーストラリア・ハマースレイ地域の縞状鉄鉱床中に胚胎する高品位鉄鉱床の下盤頁岩の熱水変質について--全岩化学組成,同位体組成,流体包有物による検討
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