Concordant and discordant podiform chromitites in the Zambales Ophiolite Complex, Philippines
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概要
- 論文の詳細を見る
- 2011-09-05
著者
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PAYOT Betchaida
Department of Earth Sciences, Kanazawa University
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ARAI Shoji
Department of Earth Sciences, Kanazawa University
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Tamayo Rodolfo
National Institute Of Geological Sciences University Of The Philippines
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Arai Shoji
Kanazawa Univ. Kanazawa Jpn
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PAYOT Betchaida
Kanazawa University
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Arai Shoji
Kanazawa University
関連論文
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- フィリピン,アンティークオフィオライトの岩石化学:火山成塊状硫化物およびポディフォームクロミタイト鉱床に対する意義
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- Preface
- Corona structure from arc mafic-ultramafic cumulates : The role and chemical characteristics of late-magmatic hydrous liquids
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- Geochemical characteristics of chloritization of mafic crust from the northern Oman ophiolite : Implications for estimating the chemical budget of hydrothermal alteration of the oceanic lithosphere
- Ca-metasomatism in the oceanic mantle as the result of high-T hydrothermal circulation : evidence from diopsidite dykes in the Oman ophiolite
- Concordant and discordant podiform chromitites in the Zambales Ophiolite Complex, Philippines
- Abyssal harzburgite veined by silica-oversaturated melt in the Sibuyan Ultramafics, Romblon, Central Philippines
- Low-temperature Sr enrichment in mantle pyroxenes as a result of crustal alteration in plagioclase lherzolite
- Clinopyroxene-rich lherzolite xenoliths from Bir Ali, Yemen - Possible product of peridotite/melt reactions