{"@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/1390282681521599232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2465/jmps.120801b"}},{"identifier":{"@type":"COI","@value":"1:CAS:528:DC%2BC3sXosFKlsb8%3D"}},{"identifier":{"@type":"NAID","@value":"10031138457"}}],"dc:title":[{"@language":"en","@value":"The spatial variation of initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios in the Toki granite, Central Japan: Implications for the intrusion and cooling processes of a granitic pluton"},{"@value":"The spatial variation of initial 87Sr/86Sr ratios in the Toki granite, Central Japan: Implications for the intrusion and cooling processes of a granitic pluton"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The spatial variation in initial <sup>87</sup>Sr/ <sup>86</sup>Sr ratios (SrI) in the Toki granite, Central Japan, shows heterogeneity ranging from 0.708942 to 0.710069, which provides information on the intrusion and cooling processes of plutons. The Toki granite has three mineralogy-based rock facies: muscovite-biotite granite (MBG), hornblende-biotite granite (HBG) and biotite granite (BG). Large SrI values were found to be distributed at the western margin (west MBG) and the lithologically central region (central BG), while small SrI values were found at the northeast margin (northeast MBG). Regions with high and low Sr concentrations were also found in the Toki granite. In the Sr-rich samples, SrI (0.708942-0.709789) increases with 100/Sr (0.7-1.5). This geochemical trend extends towards the country sedimentary rocks of the Mino Terrane, which can be interpreted to result from assimilation and fractional crystallization (AFC) between the original granitic magma and the Mino sedimentary rocks. The SrI values in the Sr-rich regions show a correlation with the Alumina Saturation Index (ASI). In particular, the west MBG, with large SrI values, is classified as a peraluminous granitoid with large ASI, suggesting that the western margin of the pluton was strongly affected by assimilation during the intrusion process. The Sr-poor samples are present both in the central BG, with large SrI values, and in the northeast MBG, with small SrI values. The Sr-poor samples have small ASI and large differentiation indices, indicating that the central BG and the northeast MBG were generated either by different AFC process with different amounts of contaminants or by the intrusion and fractionation of different source magma with different SrI values. Overall, the geochemical spatial variations found in the Toki granite can be explained by various degrees of assimilation and fractional crystallization in the magma chamber and/or multi-stage intrusions with different degrees of crystallization of plural source magmas with different SrI values. Previous petrographical and thermochronological studies revealed that the Toki granite effectively cooled from the wall at the western margin in the cooling stage at temperatures below 500 °C. Larger SrI and ASI values found in this study corresponded to the western margins where the earlier and more rapid cooling took place, indicating that the Toki granite was preferentially cooled from the peraluminous marginal regions where the assimilation of country rock was the most extensive."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801193987840","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10421679"},{"@type":"NRID","@value":"1000010421679"},{"@type":"NRID","@value":"9000000162027"},{"@type":"NRID","@value":"9000242252747"},{"@type":"NRID","@value":"9000240048587"},{"@type":"NRID","@value":"9000411228065"},{"@type":"NRID","@value":"9000017048551"},{"@type":"NRID","@value":"9000347082364"},{"@type":"NRID","@value":"9000010696198"},{"@type":"NRID","@value":"9000006337913"},{"@type":"NRID","@value":"9000411228692"},{"@type":"NRID","@value":"9000404815624"},{"@type":"NRID","@value":"9000248249024"},{"@type":"NRID","@value":"9000356565200"},{"@type":"NRID","@value":"9000322100793"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/tadahiko"}],"foaf:name":[{"@language":"en","@value":"TSURUTA Tadahiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Mizunami Underground Research Laboratory, Geological Isolation Research and Development Directorate, Japan Atomic Energy Agency"}]},{"@id":"https://cir.nii.ac.jp/crid/1410009221187064192","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000392107928"},{"@type":"NRID","@value":"9000309171326"},{"@type":"NRID","@value":"9000283905404"},{"@type":"NRID","@value":"9000392129897"},{"@type":"NRID","@value":"9000392095914"},{"@type":"NRID","@value":"9000392095784"},{"@type":"NRID","@value":"9000409173389"},{"@type":"NRID","@value":"9000392107944"},{"@type":"NRID","@value":"9000392097541"},{"@type":"NRID","@value":"9000391688983"},{"@type":"NRID","@value":"9000392121713"},{"@type":"NRID","@value":"9000009461785"},{"@type":"NRID","@value":"9000392090851"},{"@type":"NRID","@value":"9000345448644"},{"@type":"NRID","@value":"9000258222978"},{"@type":"NRID","@value":"9000258305450"},{"@type":"NRID","@value":"9000248249025"},{"@type":"NRID","@value":"9000392095743"},{"@type":"NRID","@value":"9000392095890"},{"@type":"NRID","@value":"9000240100536"},{"@type":"NRID","@value":"9000392095800"},{"@type":"NRID","@value":"9000004626328"},{"@type":"NRID","@value":"9000244901495"},{"@type":"NRID","@value":"9000392107931"},{"@type":"NRID","@value":"9000392107920"},{"@type":"NRID","@value":"9000392120639"},{"@type":"NRID","@value":"9000392095811"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/OtHjPSzdQfxWsMgBJwou"}],"foaf:name":[{"@language":"en","@value":"HAMA Katsuhiro"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Mizunami Underground Research Laboratory, Geological Isolation Research and Development Directorate, Japan Atomic Energy Agency"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681521599235","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000248249026"}],"foaf:name":[{"@language":"en","@value":"NISHIYAMA Tadao"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681521599234","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000248249023"}],"foaf:name":[{"@language":"en","@value":"YUGUCHI Takashi"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Mizunami Underground Research Laboratory, Geological Isolation Research and Development Directorate, Japan Atomic Energy Agency"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13456296"},{"@type":"LISSN","@value":"13456296"},{"@type":"EISSN","@value":"13493825"},{"@type":"NCID","@value":"AA11460926"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"},{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"}],"dc:publisher":[{"@language":"en","@value":"Japan Association of Mineralogical Sciences"},{"@language":"ja","@value":"一般社団法人　日本鉱物科学会"}],"prism:publicationDate":"2013","prism:volume":"108","prism:number":"1","prism:startingPage":"1","prism:endingPage":"12"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","availableAt":"2013","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Initial%20%3Csup%3E87%3C/sup%3ESr/%3Csup%3E86%3C/sup%3ESr%20ratio%20(SrI)","dc:title":"Initial <sup>87</sup>Sr/<sup>86</sup>Sr ratio (SrI)"},{"@id":"https://cir.nii.ac.jp/all?q=Granitic%20pluton","dc:title":"Granitic pluton"},{"@id":"https://cir.nii.ac.jp/all?q=Assimilation","dc:title":"Assimilation"},{"@id":"https://cir.nii.ac.jp/all?q=Fractional%20crystallization","dc:title":"Fractional crystallization"},{"@id":"https://cir.nii.ac.jp/all?q=Cooling%20process","dc:title":"Cooling process"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001337929890304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Thermochronology and the three-dimensional cooling pattern of a granitic pluton : An example from the Toki granite, Central Japan."},{"@value":"Thermochronology and the three-dimensional cooling pattern of a granitic pluton: an example of the Toki granite, Central Japan"},{"@value":"Thermochronology and the three-dimensional cooling pattern of a granitic pluton: An example of the Toki granite"},{"@value":"Theremochronology and the three-dimensional cooling pattern of granitic pluton: an example of the Toki granite, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050573243326441984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Position-by-position cooling paths within the Toki granite, central Japan; Constraints and the relation with fracture population in a pluton"},{"@language":"ja","@value":"土岐花崗岩体内部の冷却履歴の位置的な相違; 相違をもたらす原因と割れ目との関連"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235462535424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep microbial life in high‐quality granitic groundwater from geochemically and geographically distinct underground boreholes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429430274560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of tributary–mainstem migration of freshwater fishes by\n                    <scp>Sr</scp>\n                    isotope analysis of otoliths"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286992049548800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Crystallization processes of quartz in a granitic magma: Cathodoluminescence zonation pattern controlled by temperature and titanium diffusivity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620539637248","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Oxygen isotope evidence for crustal assimilation and magma mixing in the Granite Harbour Intrusives, Northern Victoria Land, Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620930095744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A petrological and RbSr isotopic study of an early Archean fertile granite-pegmatite system: The Sinceni Pluton in Swaziland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643820882944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mass transfer associated with chloritization in the hydrothermal alteration process of granitic pluton"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168117736960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution of the apatite fission‐track ages in the <scp>T</scp>oki granite, central <scp>J</scp>apan: <scp>E</scp>xhumation rate of a <scp>C</scp>retaceous pluton emplaced in the <scp>E</scp>ast <scp>A</scp>sian continental margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093465866368","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"RbSr dating of acidic rocks from the middle part of the Inner Zone of southwest Japan: tectonic implications for the migration of the Cretaceous to Paleogene igneous activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094334364672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal contamination and crystal entrapment during polybaric magma evolution at Mt. Somma–Vesuvius volcano, Italy: Geochemical and Sr isotope evidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095366140032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Cooling process of a granitic body deduced from the extents of exsolution and deuteric sub-solidus reactions: Case study of the Okueyama granitic body, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641722999296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ecological and genomic profiling of anaerobic methane-oxidizing archaea in a deep granitic environment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656160364288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Episyenite formation in the Toki granite, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663334941952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Role of micropores, mass transfer, and reaction rate in the hydrothermal alteration process of plagioclase in a granitic pluton"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518675360384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519091068032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994836804992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Enhanced responses to a DNA vaccine encoding a fusion antigen that is directed to sites of immune induction"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468826331520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The use of apatite as a record of initial 87Sr/86Sr ratios and indicator of magma processes in the Inagawa pluton, Ryoke belt, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471205117440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Initial 87Sr/86Sr ratios of plutonic rocks from Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944261263616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crustal origin of Hercynian peraluminous granitic batholiths of Central Spain: petrological, geochemical and isotopic (Sr, Nd) constraints"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945744564992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonostratigraphy of Mino terrane: Jurassic accretionary complex of southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419300978176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Heterogeneity of initial 87 Sr/ 86 Sr ratios within a single pluton: evidence from apatite strontium isotopic study"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370458878848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Denudation history of the high <i>T</i>/<i>P</i> Ryoke metamorphic belt, southwest Japan: constraints from CHIME monazite ages of gneisses and granitoids"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318281064832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE China"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320243004032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The statistical assessment of Rb-Sr isochrons"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794620481024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Isotopic and palaeomagnetic evidence for rates of cooling, uplift and erosion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794837632768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Feasibility of AFC models for the petrogenesis of calc-alkaline magma series"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204549690752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic ages of siliceous shale from Hida-Kanayama, central Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205194426880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chemical compositions of the late Cretaceous Ryoke granitoids of the Chubu District, central Japan – Revisited"},{"@language":"ja","@value":"中部地方の後期白亜紀領家帯花崗岩類の化学的性質の再検討"},{"@value":"Chemical compositions of the late Cretaceous Ryoke granitoids of the Chubu District, central Japan—Revisited"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205530787584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heterogeneity of initial 87Sr/86Sr ratio within the Kamihara Tonalite, Ryoke belt, southwest Japan: Implications for the wall rock assimilation"},{"@language":"ja","@value":"中部地方領家帯神原トーナライトにおけるSr同位体初生値の不均質と同化作用"},{"@value":"Initial 87Sr/86Sr ratio heterogeneity in Kamihara Tonalite, Ryoke belt, southwest Japan: Evidence from strontium isotopic analysis of apatite"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237412608","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Formative periods and source materials of Cretaceous-Paleogene granitoids from Honshu Arc"},{"@language":"ja","@value":"本州弧に分布する白亜紀～古第三紀花崗岩の活動と起源物質"},{"@language":"ja-Kana","@value":"ホンシュウ コ ニ ブンプ スル ハクアキ コ ダイ3キ カコウガン ノ カツドウ ト キゲン ブッシツ"},{"@value":"Formative periods and source materials of Cretaceous-Paleogene granitoids from Honsyu Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237431936","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Rb-Sr GEOCHRONOLOGICAL STUDY OF THE RYOKE GRANITES IN CHUBU DISTRICT, CENTRAL JAPAN"},{"@value":"中部地方・領家花こう岩の Rb-Sr 法による地質年代学的研究"},{"@language":"ja-Kana","@value":"チュウブ チホウ リョウケ カコウガン ノ Rb-Srホウ ニ ヨル チシツ ネンダイガクテキ ケンキュウ エイブン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545340160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zircon growth in a granitic pluton with specific mechanisms, crystallization temperatures and U–Pb ages: Implication to the ‘spatiotemporal’ formation process of the Toki granite, central Japan"},{"@value":"Zircon growth in a granitic pluton with specific mechanisms, crystallization temperature and U-Pb ages: implication to the ‘spatiotemporal’ formation process of the Toki granite, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545948160","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional cooling pattern of a granitic pluton I: The study of exsolution sub-solidus reactions in the Toki granite, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277396875776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"岐阜県恵那市明智町東方及びその周辺地域に産する花崗岩類の全岩主成分・微量成分組成とその帰属"},{"@language":"en","@value":"Whole-rock major and trace element geochemistry and geotectonic attribution of granitic rocks around the Higashigata, Akechi Town, Ena City, Gifu Prefecture, central Japan"},{"@language":"ja-Kana","@value":"ギフケン エナシ アケチマチ トウホウ オヨビ ソノ シュウヘン チイキ ニ サンスル カコウガンルイ ノ ゼン ガン シュセイブン ・ ビリョウ セイブン ソセイ ト ソノ キゾク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390009224404306176","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An 85 ± 5 Ma CHIME age for the Agigawa welded tuff sheet in the oldest volcanic sequence of the Nohi Rhyolite, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679211005440","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"白神山地の花崗岩類と東北地方の白亜紀-古第三紀花崗岩類との対比"},{"@language":"en","@value":"On the granitoids in the Shirakami mountains and correlation to the Cretaceous to Palaeogene granitoids distributed in the Northeast Japan"},{"@language":"ja-Kana","@value":"シラカミ サンチ ノ カコウガンルイ ト トウホク チホウ ノ ハクアキ コ ダイ3キ カコウガンルイ ト ノ タイヒ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679527010176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rb-Sr whole-rock and K-Ar mineral ages of granitic rocks in Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679527394816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic ages of Jurassic siliceous shale and Triassic bedded chert in Unuma, Central Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680171265920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"山陽帯と領家帯の白亜紀後期花崗岩類の化学的性質の対照性：岡山南部-香川断面の場合"},{"@language":"en","@value":"Chemical contrast of the Late Cretaceous granitoids of the Sanyo and Ryoke Belts, Southwest Japan: Okayama-Kagawa Transect."},{"@value":"Chemical contrast of the Late Cretaceous grantitoids of the Sanyo and Ryoke Belts, Southwest Japan: Okayama-Kagawa Transect"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211277568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fracture analysis of the Toki Granite in the Tono district, central Japan."},{"@value":"中部日本東濃地方，土岐花こう岩中の割れ目解析"},{"@language":"ja-Kana","@value":"チュウブ ニホン トウノウ チホウ トキ カコウガン チュウ ノ ワレメ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502465536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zoning of rock facies and chemical composition in the Toki granitic body, Central Japan"},{"@language":"ja","@value":"中部日本土岐花崗岩体の岩相と化学組成の累帯変化"},{"@language":"ja-Kana","@value":"チュウブ ニホン トキ カコウガンタイ ノ ガンソウ ト カガク ソセイ ノ ルイタイ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681503160064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cooling history of the Cretaceous Toki granite in the eastern Sanyo Belt, Central Japan"},{"@language":"ja","@value":"山陽帯東部，土岐花崗岩体の冷却史"},{"@language":"ja-Kana","@value":"サンヨウタイ トウブ,トキ ハナオカガンタイ ノ レイキャクシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681521723136","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional cooling pattern of a granitic pluton II: The study of deuteric sub-solidus reactions in the Toki granite, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1520853834181087616","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Chemical compositions of the late Cretaceous Ryoke granitoids of the Chubu District, central Japan: revisited"},{"@language":"ja-Kana","@value":"Chemical compositions of the late Cretaceous Ryoke granitoids of the Chubu District central Japan revisited"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009751427977600","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rb-Sr whole-rock and K-Ar mineral ages of granitic rocks in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009751427978880","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chemical contrast of the Late Cretaceous granitoids of the Sanyo and Ryoke Belts, Southwest Japan : Okayama-Kagawa Transect"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009751427981184","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic and paleomagnetic evidence for rates of cooling, uplift and erosion"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291226404686720","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Denudation history of the high T/P Ryoke metamorphic belt, southwest Japan : constraints from CHIME monazite ages of gneisses and granitoids"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291226404687872","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570291226404692992","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cooling process of a granitic body deduced from the extents of exsolution and deuteric sub-solidus reactions : Case study of the Okueyama granitic body, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701381397760","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Subcommission on Geochronology : Convention on the use of decay constants in geo- and cosmochronology"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701381398912","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal origin of Hercynian peraluminous granitic batholiths of Central Spain : petrological, geochemical and isotopic (Sr, Nd) constraints"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701381400064","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology of the Mizunami district, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572701381401216","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1570572701381402368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Feasibility of AFC models for the petrogenesis of calc-alkaline magma series"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854176358109056","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE China"}]},{"@id":"https://cir.nii.ac.jp/crid/1571135651334822016","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic ages of siliceous shale from Hida-Kanayama, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417126311529088","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Thermochronology and the three-dimensional cooling pattern of a granitic pluton : An example of the Toki granite, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417126311530240","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology of the Mizunami district, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571417126311534720","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Oxygen isotope evidence for crustal assimilation and magma mixing in the Granite Harbour Intrusives, Northern Victoria Land, Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698601288239488","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A petrological and Rb-Sr isotopic study of an early Archean fertile granite-pegmatite system : the Sinceni Pluton in Swaziland"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698601288240768","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Isotopic ages of Jurassic siliceous shale and Triassic bedded chert in Unuma, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1571698601288242560","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rb-Sr dating of acidic rocks from the middle part of the Inner Zone of southwest Japan : tectonic implications for the migration of the Cretaceous to Paleogene igneous activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1572261551241664768","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1572261551241665920","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rb-Sr whole-rock isochron ages and Sr isotopic ratios of the Nohi Rhyolite"},{"@value":"Rb‐Sr whole‐rock isochron ages and Sr isotopic ratios of the Nohi Rhyolite"}]},{"@id":"https://cir.nii.ac.jp/crid/1572543026218374400","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heterogeneity of initial ^<87>Sr/^<86>Sr ratios within a single pluton : evidence from apatite strontium isotopic study"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824501195082496","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3D Geological Modelling in Regional Hydrogeological Study in the Tono Area"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824501195088512","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573105976171794688","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573105976171798272","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonostratigraphy of Mino terrane : Jurassic accretionary complex of southwest Japan. Palaeogeography, Palaeoclimatology"}]},{"@id":"https://cir.nii.ac.jp/crid/1573387451148508928","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fracture analysis of the Toki Granite in the Tono district, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668926125217024","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Initial ^<87>Sr/^<86>Sr ratio ratios of plutonic rocks from Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668926125220480","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1573950401101927296","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The statistical assessment of Rb-Sr isochrons"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401101929728","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The use of apatite as a record of initial ^<87>Sr / ^<86>Sr ratios and indicator of magma processes in the Inagawa pluton, Ryoke belt, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1573950401101931136","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231876078635136","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal contamination and crystal entrapment during polybaric magma evolution at Mt. Somma-Versuvius volcano, Italy : Geochemical and isotope evidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1574231876078637696","@type":"Article","relationType":["cites"]},{"@id":"https://cir.nii.ac.jp/crid/1574231876078641280","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zoning of rock facies and chemical composition in the Toki granitic body, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942186668032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volatile (F and Cl) concentrations in Iwate olivine-hosted melt inclusions indicating low-temperature subduction"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:1001554653"},{"@type":"CROSSREF","@value":"10.2465/jmps.120801b"},{"@type":"CIA","@value":"10031138457"},{"@type":"OPENAIRE","@value":"doi_dedup___::b6d8c7041d6930d8256a2163a53eccf6"},{"@type":"CROSSREF","@value":"10.1111/1758-2229.12379_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1111/1440-1703.12531_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.2138/am-2020-7353_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.70.335_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1111/iar.12219_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1038/ismej.2017.140_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1007/s00410-013-0960-8_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.2138/am-2019-6786_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.2465/jmps.151007_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-81_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2020.104289_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"},{"@type":"CROSSREF","@value":"10.1016/j.jseaes.2018.07.039_references_DOI_TiP1lmYxIq7rliIiy0qJYaOd7lm"}]}