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
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概要
- 論文の詳細を見る
- 日本鉱物科学会の論文
- 2009-06-01
著者
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Ishida Yoshito
Department Of Earth Sciences Kanazawa University
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Ishida Yoshito
Department Of Earth Sciences Faculty Of Sciences Kanazawa University
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Arai Shoji
Earth Science Course School Of Natural System College Of Science And Engineering Kanazawa University
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TAMURA AKIHIRO
Frontier Science Organization, Kanazawa University
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Tamura Akihiro
Earth Science Course School Of Natural System College Of Science And Engineering Kanazawa University
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YOSHITAKE Naoya
Division of Earth and Environmental Sciences, Natural Science and Technology Kanazawa University
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Arai Shoji
Faculty Of Science Department Of Earth Science Kanazawa University
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Arai Shoji
Kanazawa University
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Tamura Akihiro
Frontier Science Organization Kanazawa University
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Yoshitake Naoya
Division Of Earth And Environmental Sciences Natural Science And Technology Kanazawa University
関連論文
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- Constraints on the evolutionary history of aluminous mafic rocks in the Ronda peridotite massif (Spain) from trace-element compositions of clinopyroxene and garnet
- Trace element compositions of jadeite (+omphacite) in jadeitites from the Itoigawa-Ohmi district, Japan: Implications for fluid processes in subduction zones
- Podiform chromitites in the lherzolite-dominant mantle section of the Isabela ophiolite, the Philippines
- Simultaneous determination of multiple trace element compositions in thin(
- The solution introduction ICP-MS technique to trace element analysis of rocks
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- Subarc magmatic and hydration processes inferred from a hornblende peridotite xenolith in spessartite from Kyoto, Japan
- Genesis of peculiarly zoned Co, Zn and Mn-rich chromian spinel in serpentinite of Bou-Azzer ophiolite, Anti-Atlas, Morocco
- Trace element and Sr-Nd isotopic features of ultramafic xenoliths from Kurose, Southwest Japan
- Trace element heterogeneity in hydrothermal diopside: Evidence for Ti depletion and Sr-Eu-LREE enrichment during hydrothermal metamorphism of mantle harzburgite
- Petrology of the Yugu peridotites in the Gyeonggi Massif, South Korea: Implications for its origin and hydration process
- 40Ar-39Ar analysis of phlogopite in the Horoman Peridotite Complex, Hokkaido, Japan and implications for its origin
- Geochemistry of clinopyroxene in peridotites from the Nukabira complex, Kamuikotan zone, Hokkaido, Japan : a LA-ICP-MS study
- Corona structure from arc mafic-ultramafic cumulates : The role and chemical characteristics of late-magmatic hydrous liquids
- Inhomogeneous spinel in chromitite from the Iwanai-dake peridotite complex, Hokkaido, Japan : variations of spinel unmixing texture and chemical composition
- 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
- Crustal diopsidites from the northern Oman ophiolite : Evidence for hydrothermal circulation through suboceanic Moho
- Low-temperature Sr enrichment in mantle pyroxenes as a result of crustal alteration in plagioclase lherzolite