{"@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/1390001204304179072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.18940/kazan.45.3_149"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"5465261"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/5465261"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I5465261"}},{"identifier":{"@type":"NAID","@value":"110003041188"}}],"dc:title":[{"@language":"ja","@value":"東伊豆単成火山群における珪長質マグマの成因"},{"@language":"en","@value":"Petrogenesis of Felsic Magma in Higashi-Izu Monogenetic Volcano Group"},{"@language":"ja-Kana","@value":"ヒガシイズタンセイカザングン ニ オケル ケイチョウシツ マグマ ノ セイイン"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The activity of Higashi-Izu monogenetic volcano group produced basalt, andesite, dacite, and rhyolite, which can be classified into rock types by whole-rock composition and phenocryst assemblage. It has been widely accepted that felsic upper crust has an important role in forming compositionally diverse ejecta; andesites are formed through the assimilation of felsic crust by the basaltic magma and the felsic magmas through remelting of the felsic crust. To reinvestigate genesis of felsic magma, I examine the physicochemical conditions of both pre-eruption felsic magmas and the felsic crust. Beside observed rhyolite, felsic magmas can be recognized in dacite as endmember of magma mixing. The pairs of the magnetite and ilmenite yield the temperature of 820-790℃ for the rhyolite and 850-820℃ for the dacite. The plagioclase geohydrometer shows that the rhyolitic magmas had PH20 of 2 kbar indicating their residence within the felsic upper crust at the depth of 6-15 km before eruption. Some andesite could be formed through bulk assimilation, a simple mixing between felsic crust and basaltic magma. The compositions of the felsic crust are obtained using mixing ratios of the felsic crust and basalt magrna. The felsic crust which could range from rhyolitic to andesitic, differs from those of the rhyolitic magmas; the rhyolitic magrnas are lower in HREE (Gd, Er, Dy) and Sr, and higher in LILE (Rb, Ba, K<sub>2</sub>O) than those of the felsic crust. In addition, rhyolitic magmas cannot be formed by the fractional crystallization from the magma formed by the remelting of the felsic crust; Rb/K<sub>2</sub>O ratio of the rhyolitic magmas is higher than that of the felsic crust. However, partial melting of the felsic crust, leaving amphibole and plagioclase as the residue could produce the rhyolitic magmas."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276180615424","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00374918"},{"@type":"NRID","@value":"1000000374918"},{"@type":"NRID","@value":"9000391401017"},{"@type":"NRID","@value":"9000258434687"},{"@type":"NRID","@value":"9000000487021"},{"@type":"NRID","@value":"9000401696659"},{"@type":"NRID","@value":"9000380980702"},{"@type":"NRID","@value":"9000380981213"},{"@type":"NRID","@value":"9000403036367"},{"@type":"NRID","@value":"9000380981229"},{"@type":"NRID","@value":"9000258165449"},{"@type":"NRID","@value":"9000263067812"},{"@type":"NRID","@value":"9000380981569"},{"@type":"NRID","@value":"9000263067870"},{"@type":"NRID","@value":"9000380980705"},{"@type":"NRID","@value":"9000345426815"},{"@type":"NRID","@value":"9000380981249"},{"@type":"NRID","@value":"9000015568461"},{"@type":"NRID","@value":"9000400162075"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/microlite"}],"foaf:name":[{"@language":"ja","@value":"鈴木 由希"},{"@language":"en","@value":"SUZUKI Yuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"},{"@language":"ja","@value":"東京大学地震研究所"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04534360"},{"@type":"EISSN","@value":"21897182"},{"@type":"NDL_BIB_ID","@value":"000000003812"},{"@type":"ISSN","@value":"04534360"},{"@type":"LISSN","@value":"04534360"},{"@type":"NCID","@value":"AN10512786"}],"prism:publicationName":[{"@language":"en","@value":"BULLETIN OF THE VOLCANOLOGICAL SOCIETY OF JAPAN"},{"@language":"ja","@value":"火山"},{"@language":"en","@value":"BVSJ"}],"dc:publisher":[{"@language":"en","@value":"The Volcanological Society of Japan"},{"@language":"ja","@value":"特定非営利活動法人 日本火山学会"}],"prism:publicationDate":"2000","prism:volume":"45","prism:number":"3","prism:startingPage":"149","prism:endingPage":"171"},"url":[{"@id":"http://id.ndl.go.jp/bib/5465261"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I5465261"}],"availableAt":"2000","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360574094714926976","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Rare Earth Elements in Petrogenetic Studies of Igneous Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470857333888","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Partition coefficients for trace elements in silicic magmas"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419580359424","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Melting experiments on hydrous low‐K tholeiite: Implications for the genesis of tonalitic crust in the Izu–Bonin – Mariana arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266591744","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"伊豆・天城火山群の岩石学的および化学的性質"},{"@language":"en","@value":"Petrology and Chemistry of the Amagi Volcanic Rocks, Izu Peninsula, Japan"},{"@language":"ja-Kana","@value":"イズ アマギ カザングン ノ ガンセキガクテキ オヨビ カガクテキ セイシツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525953536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of volcanic rocks in the Tanzawa-Oiso area, central Japan: Implication for westward migration of the Pliocene volcanic front in the southern Fossa Magna region"},{"@language":"ja","@value":"丹沢-大磯地域に分布する火山岩類の K-Ar 年代と南部フォッサマグナ地域における鮮新世火山フロントの西方移動"},{"@language":"ja-Kana","@value":"タンザワ-オオイソ チイキ ニ ブンプ スル カザンガンルイ ノ K-Ar ネンダイ ト ナンブ フォッサマグナ チイキ ニ オケル センシンセイ カザン フロント ノ サイホウ イドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009224802882688","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"伊豆半島東方沖ドレッジ試料の岩石学的研究"},{"@language":"ja-Kana","@value":"イズ ハントウ トウホウオキ ドレッジ シリョウ ノ ガンセキガクテキ ケンキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009226038073728","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"The Higashi-Izu-oki Submarine Volcanoes, Part 1"},{"@language":"ja","@value":"東伊豆沖海底火山群 : その1"},{"@language":"ja-Kana","@value":"ヒガシ イズオキ カイテイ カザングン 1"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679133042944","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"伊豆弧の火山から噴出するマグマ中のウラン系列核種間の放射平衡・非平衡"},{"@language":"en","@value":"Radioactive Equilibria and Disequilibria of U-Series Nuclides in Erupting Magmas from Izu Arc Volcanoes"},{"@language":"ja-Kana","@value":"イズ コ ノ カザン カラ フキダスル マグマ チュウ ノ ウラン ケイレツカクシュ カン ノ ホウシャ ヘイコウ ヒヘイコウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280642816","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東伊豆単成火山地域の噴火史1:0～32ka"},{"@language":"en","@value":"Eruptive History of the Higashi Izu Monogenetic Volcano Field 1:0-32ka"},{"@language":"ja-Kana","@value":"ヒガシ イズ タンセイ カザン チイキ ノ フンカシ 1 0 32ka"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280698624","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東伊豆単成火山群岩ノ窪火山の<sup>14</sup>C年代"},{"@language":"en","@value":"<sup>14</sup>C Age of the Iwanokubo Volcano, Higashi-Izu Monogenetic Volcano Group"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679281162368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東伊豆単成火山地域の噴火史2 : 主として32ka以前の火山について(＜特集＞堆積物による火山噴火史研究)"},{"@language":"en","@value":"Eruptive History of the Higashi-Izu Monogenetic Volcano Field 2 : Mainly on Volcanoes Older than 32,000 Years Ago(＜Special Section＞Volcanic History and Eruptive Deposits)"},{"@value":"東伊豆単成火山地域の噴火史-2-主として32ka以前の火山について"},{"@language":"ja-Kana","@value":"ヒガシ イズ タンセイ カザン チイキ ノ フンカシ 2 シュ ト シテ 32"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681097646976","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"富士・箱根・伊豆地域火山岩類のストロンチウム同位体組成"},{"@language":"en","@value":"Isotopic Composition of Strontium in Volcanic Rocks from Fuji, Hakone, and Izu Area, Central Japan"},{"@language":"ja-Kana","@value":"フジ ハコネ イズ チイキ カザンガンルイ ノ ストロンチウム ドウイタイ ソ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390572175991548160","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"The Subcrustal Discontinuity with a Molten Material at the East Coast off the Izu Peninsula"},{"@language":"ja","@value":"伊豆半島東岸の溶融体を伴う地殻深部不連続面"},{"@language":"ja-Kana","@value":"イズ ハントウ トウガン ノ ヨウユウタイ オ トモナウ チカク シンブ フレ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390853650975745152","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"21. The Higashi-Izu-oki Submarine Volcanoes, Part 2, and the Submarine Volcanoes near the Izu Shoto Islands"},{"@language":"ja","@value":"21. 東伊豆沖海底火山群 : その2-および伊豆諸島近海海底火山"},{"@language":"ja-Kana","@value":"ヒガシ イズオキ カイテイ カザングン 2 オヨビ イズ ショトウ キンカイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520009408653580032","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"珪酸塩岩の蛍光X線分析-1-主成分の分析"},{"@language":"ja-Kana","@value":"ケイサンエンガン ノ ケイコウ Xセン ブンセキ 1 シュセイブン ノ ブンセ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520290882230727680","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"珪酸塩岩の蛍光X線分析-2-微量元素の分析"},{"@language":"ja-Kana","@value":"ケイサンエンガン ノ ケイコウ Xセン ブンセキ 2 ビリョウ ゲンソ ノ ブ"}]},{"@id":"https://cir.nii.ac.jp/crid/1520853835167586688","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"東伊豆単成火山群の岩石〔英文〕"},{"@language":"ja-Kana","@value":"ヒガシイズ タンセイ カザングン ノ ガンセキ エイブン"}]},{"@id":"https://cir.nii.ac.jp/crid/1521699229941228928","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"東伊豆単成火山群の岩石学--捕獲結晶の意義と噴出物の時空的変化"},{"@language":"ja-Kana","@value":"ヒガシ イズ タンセイ カザングン ノ ガンセキガク ホカク ケッショウ ノ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009750904474112","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Generation of metaluminous A-type granites by low-pressure melting of calc-alkaline granitoids"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009751068263808","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrogenesis of the Tanzawa plutonic complex, central Japan : Exposed felsic middle crust of the Izu-Bonin-Mariana arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009751736177664","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic zonations in silicic magma chambers."}]},{"@id":"https://cir.nii.ac.jp/crid/1570291226731880576","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diversity of parent magmas of Higashi-Izu monogenetic volcano group."}]},{"@id":"https://cir.nii.ac.jp/crid/1570572699136013312","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"1989年7月の伊豆半島東方沖海底火山噴火と噴出物"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701506698240","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Colima Volcanic Complex, Mexico. I. post-caldera andesites from Volcan Colima"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701512233088","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The application of trace elements to the petrogenesis of igneous rocks of granitic composition."}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701709825280","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dyke intrusion model for the 1989 seismovolcanic activity off Ito, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701761712768","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Groundmass pargasite in the 1991-1995 dacite of Unzen volcano : phase stability experiments and volcanological implications"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175837227264","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Experimental constarints on differentiation and H_2O abundance of calc-alkaline magmas."}]},{"@id":"https://cir.nii.ac.jp/crid/1570854176670580992","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Assimilation of granite by basaltic magma at Burnt Lava flow, Medicine Lake volcano, northern California:Decoupling of heat and mass transfer."}]},{"@id":"https://cir.nii.ac.jp/crid/1570854176679576576","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The May 18, 1980, eruption of Mount St. Helens. 1. Melt composition and experimental phase equilibria"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135649048575616","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sr/Ca-Ba/Ca systematics in Higashi-Izu monogenetic Volcano group, Izu Peninsula, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1571135649249018112","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"関東山地三波川変成帯の塩基性岩類の全岩分析による地球化学的研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135649249036416","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology and petrology of Omuroyama volcano group, north Izu"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124066184064","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"伊豆半島大室山天城側火山群地久保中央火口丘降下スコリア, カワゴ平火砕流の^<14>C年代"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417124225747584","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Partition coefficients determined from phenocryst and glass analyses of the climactic ejecta of Mount Mazama, Oregon."}]},{"@id":"https://cir.nii.ac.jp/crid/1571417126627080320","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dissolution kinetics of plagioclase in the melt of the system diopside-albite-anorthite, and origin of dusty plagioclase in andesites"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698599001088384","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Trace element geochemistry of high alumina basalt-andesite-dacite-rhyodacite lavas of the Main Volcanic Series of Santorini Volcano, Greece"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698601601161216","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent volcanism in the Puyehue-Cordon Caulle Region, southern Andes, Chile(40.5°S):petrogenesis of evolved lavas."}]},{"@id":"https://cir.nii.ac.jp/crid/1571980074010303360","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1571980074052931968","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-alumina basalt."}]},{"@id":"https://cir.nii.ac.jp/crid/1572261549155861504","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diffusion coronas around quartz xenocrysts in andesites and basalt from tertiary volcanic region in northeastern Shikoku, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1572261551595254912","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origin of compositional zonation(high alumina basalt to basaltic andesite)in the Giant Crater lava field, Medicine Lake volcano, northern California."}]},{"@id":"https://cir.nii.ac.jp/crid/1572543026347292160","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Iron (II)-magnesium exchange between olivine and calcium-free pyroxene over a temperature range 800℃ to 1300℃"}]},{"@id":"https://cir.nii.ac.jp/crid/1572543026350092160","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal structure in the northern part of the Philippine Sea plate as derived from seismic observations of Hatoyama-off Izu Peninsula explosions"}]},{"@id":"https://cir.nii.ac.jp/crid/1573105973959941248","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cosmochemistry of the rare earth elements: meteorite studies."}]},{"@id":"https://cir.nii.ac.jp/crid/1573387448865046656","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal structure in Izu Peninsula, Central Japan, as derived from explosion seismic observations 1. Mishima-Shimoda profile"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387448887869056","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Empirical correction factors for the electron microanalysis of silicates and oxides"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387449062703232","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Experimental studies of igneous rock series:A zoned pluton in the Wallowa Batholith, Oregon."}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451476386432","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Plagioclase-melt equilibria in hydrous systems."},{"@value":"Plagioclase‐melt equilibria in hydrous system"},{"@value":"Plagioclase‐melt equilibria in hydrous systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668926427197568","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mg/Mn partitioning as test for equilibrium between coexisting Fe-Ti oxides"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950398818704128","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Phase equilibriua of rock-forming ferromagnesian silicates in granitic systems."}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401230845952","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The iron-magnesium partitioning between naturally occurring coexisting olivine and Ca-rich clinopyroxene:an application of the simple mixture model to olivine solid solution"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401452816896","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The South Fossa, Magna, Japan, revealed by high-resolution P-and S-wave travel time tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231876405856384","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Why does the Higashi-Izu monogenetic volcano group exist in the Izu peninsula? : Relationships between late Quaternary volcanism and tectonics in the northern tip of the Izu-Bonin arc."}]},{"@id":"https://cir.nii.ac.jp/crid/1574231876429862784","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fe-Ti oxide geothermometry : thermodynamic formulation and the estimation of intensive variables in silicic magmas"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2001960031"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I5465261"},{"@type":"CIA","@value":"110003041188"}]}