{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360004239506177024.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.3390/min8120583"}},{"identifier":{"@type":"URI","@value":"https://www.mdpi.com/2075-163X/8/12/583/pdf"}},{"identifier":{"@type":"HANDLE","@value":"1912/23640"}},{"identifier":{"@type":"HANDLE","@value":"11571/1231506"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Occurrence of Felsic Rocks in Oceanic Gabbros from IODP Hole U1473A: Implications for Evolved Melt Migration in the Lower Oceanic Crust"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Felsic rocks are minor in abundance but occur ubiquitously in International Ocean Discovery Program Hole U1473A, Southwest Indian Ridge. The trace element abundances of high-Ti brown amphibole, plagioclase, and zircon in veins, as well as the presence of myrmekitic texture in the studied felsic rocks support crystallization origin from highly-evolved melts, probably controlled by fractional crystallization. Based on geochemical criteria and texture of the mineral assemblage in felsic rocks and their relationship with host gabbros, they can be divided into three types: (1) Felsic rock with sharp boundaries is formed when felsic melt intrudes into fractures of host gabbros, resulting in minimal interaction between the melt and the wall minerals. (2) Replacive felsic rock, which is characterized by a pseudomorphic replacement of minerals in the host gabbro. This vein type is caused by the replacement of the host mineralogy by minerals in equilibrium with the felsic melts. (3) Felsic rock with diffused boundaries is formed either by infiltration of felsic melt into the solidifying gabbro body or crystallization of interstitial melts. Infiltration modes of felsic melts are likely controlled by the temperature condition of the cooling host gabbros.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380863721863626526","@type":"Researcher","foaf:name":[{"@value":"Du Khac Nguyen"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Natural Science and Technology, Kanazawa University, Kakuma-machi, Kanazawa Ishikawa 920-1192, Japan"},{"@value":"Faculty of Geosciences and Geoengineering, Hanoi University of Mining and Geology, Hanoi 100000, Vietnam"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177155","@type":"Researcher","foaf:name":[{"@value":"Tomoaki Morishita"}],"jpcoar:affiliationName":[{"@value":"College of Science and Engineering, Kanazawa University, Kakuma-machi, Kanazawa Ishikawa 920-1192, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177026","@type":"Researcher","foaf:name":[{"@value":"Yusuke Soda"}],"jpcoar:affiliationName":[{"@value":"College of Science and Engineering, Kanazawa University, Kakuma-machi, Kanazawa Ishikawa 920-1192, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177154","@type":"Researcher","foaf:name":[{"@value":"Akihiro Tamura"}],"jpcoar:affiliationName":[{"@value":"College of Science and Engineering, Kanazawa University, Kakuma-machi, Kanazawa Ishikawa 920-1192, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177031","@type":"Researcher","foaf:name":[{"@value":"Biswajit Ghosh"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, University of Calcutta, 35 Ballygunge Circular Road Kolkata, West Bengal 700019, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177152","@type":"Researcher","foaf:name":[{"@value":"Yumiko Harigane"}],"jpcoar:affiliationName":[{"@value":"Institute of Geology and Geoinformation, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, AIST Tsukuba Central 7, 1-1-1 Higashi, Tsukuba Ibaraki 305-8567, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177153","@type":"Researcher","foaf:name":[{"@value":"Lydéric France"}],"jpcoar:affiliationName":[{"@value":"Centre de Recherches Pétrographiques et Géochimiques (UMR 7358), CNRS, Université de Lorraine, 54501 Vandœuvre les Nancy, France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004239506177032","@type":"Researcher","foaf:name":[{"@value":"Chuanzhou Liu"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. 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