{"@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/1361699996333958016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0024-4937(88)90022-9"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0024493788900229?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0024493788900229?httpAccept=text/plain"}}],"dc:title":[{"@value":"Tholeiitic and calc-alkaline magma series at Adatara volcano, northeast Japan: 1. Geochemical constraints on their origin"}],"description":[{"notation":[{"@value":"Abstract   Low-alkali [“island arc” by Jakes and Gill (1970) or “low-K” by Gill (1978)] tholeiitic rocks are closely associated with calc-alkaline rocks in the outer volcanic zone (called the Nasu volcanic zone) of northeast Japan. Major-element, trace-element (Ni, Cr, Co, Sc, V, Zr, Nb, Zn, Rb, Cs, Ba, Sr, Ce and Y) and Sr isotope compositions are presented for 9 low-alkali tholeiitic and 16 calc-alkaline samples of Adatara volcano belonging to the Nasu volcanic zone. In the trace elements vs. SiO 2  diagram the tholeiitic series and calc-alkaline series show different trends to each other for Co, Sc, V, Zr, Rb, Sc, Ba and Sr. As expected from K 2 O contents, the calc-alkaline samples are enriched in incompatible elements such as Rb, Cs, Ba, Ce and Zr compared with the tholeiitic samples. On the other hand, contents of Nb in the calc-alkaline samples are somewhat lower than those in the tholeiitic samples. Plots of Ni and Cr contents vs. SiO 2  for the tholeiitic samples come near smooth trend lines whereas those for the calc-alkaline samples are scattered. Sr isotopic ratios in the tholeiitic series lie within the range between 0.7056 and 0.7058 and between 0.7048 and 0.7052 in the calc-alkaline series.  Smooth major- and trace-element compositional trends in the tholeiitic series are successfully modelled by simple fractional crystallization of plagioclase, hypersthene, augite, titanomagnetite and minor olivine. Similarly, crystal fractionation models can closely reproduce major- and most of the trace-element variations in the calc-alkaline series, but failed to account for irregular variations of Ni and Cr. The scattering of Ni and Cr probably reflects simultaneous crystal fractionation and (subordinate) magma mixing in the subvolcanic chamber. The inferred fractionated phases for the calc-alkaline series are richer in augite and titanomagnetite and slightly poorer in plagioclase than those for the tholeiitic series. The tholeiitic magma and calc-alkaline magma are not derived from a common parental (tholeiitic) magma and the calc-alkaline parental magma is richer in SiO 2  and incompatible elements (in particular Rb and Zr), poorer in radiogenic Sr and possibly more oxidized than the tholeiitic parental magma."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699996333958016","@type":"Researcher","foaf:name":[{"@value":"Akihiko Fujinawa"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00244937"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00244937"}],"prism:publicationName":[{"@value":"Lithos"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1988-12","prism:volume":"22","prism:number":"2","prism:startingPage":"135","prism:endingPage":"158"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0024493788900229?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0024493788900229?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360283691683362688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structure and growth of the Izu‐Bonin‐Mariana arc crust: 2. Role of crust‐mantle transformation and the transparent Moho in arc crust evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711231218944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of late Cenozoic magmatism and the crust–mantle structure in the NE Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184695144576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Primary Magmas at the Volcanic Front of the NE Japan Arc: Coeval Eruption of Crustal Low-K Tholeiitic and Mantle-derived Medium-K Calc-Alkaline Basalts at Azuma Volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568470777535104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"From sink to volcanic source: Unravelling missing terrestrial eruption records by characterization and high‐resolution chronology of lacustrine volcanic density flow deposits, Lake Inawashiro‐ko, Fukushima, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229798527744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Importance of Long-Term Shallow Degassing of Basaltic Magma on the Genesis of Massive Felsic Magma Reservoirs: a Case Study of Aso Caldera, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360849942032608384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Generation of calc-alkaline andesite magma through crustal melting induced by emplacement of mantle-derived water-rich primary magma: Evidence from Rishiri Volcano, southern Kuril Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234868736","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Genetic relationships between basalts and andesites in the Taradake volcanic area, Northwest Kyushu."},{"@language":"ja","@value":"北西九州，多良岳火山地域に分布する玄武岩類と安山岩類の成因関係"},{"@language":"ja-Kana","@value":"ホクセイ キュウシュウ タラダケ カザン チイキ ニ ブンプスル ゲンブガンル"},{"@value":"Genetic relationship between basalts and andesites in the Taradake volcanic area, Norhwest Kyushu"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206524593664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development history and changes of magma plumbing systems of Adatara volcano during recent 250000 years"},{"@language":"ja","@value":"安達太良火山の最近２５万年間における山体形成史とマグマ供給系の変遷"},{"@language":"ja-Kana","@value":"アダタラ カザン ノ サイキン 25マンネンカン ニ オケル サンタイ ケイセイシ ト マグマ キョウキュウケイ ノ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525007616","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrologic study of tholeiitic series from the Inaniwadake district, Northeast Japan arc: The high-temperatyre type tholeiitic magma erupted during Pliocene"},{"@language":"ja","@value":"東北日本弧，稲庭岳に産するソレアイト系列岩の岩石学的研究―鮮新世の噴出した高温タイプのソレアイトマグマ―"},{"@value":"東北日本弧,稲庭岳に産するソレアイト系列岩の岩石学的研究--鮮新世に噴出した高温タイプのソレアイトマグマ"},{"@language":"ja-Kana","@value":"トウホク ニホン コ イナニワダケ ニ サンスル ソレアイト ケイレツガン ノ ガンセキガクテキ ケンキュウ センシンセイ ニ フンシュツ シタ コウオン タイプ ノ ソレアイトマグマ"},{"@value":"Petrologic study of tholeiitic series from the Inaniwadake district, Northeast Japan arc: The high-temperature type tholeiitic magma erupted during Pliocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525021696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sr, Nd and Pb isotopic compositions of volcanic rocks from the Inaniwadake district, Northeast Japan arc"},{"@language":"ja","@value":"東北日本弧，稲庭岳地域の火山岩のＳｒ，Ｎｄ，Ｐｂ同位体組成"},{"@language":"ja-Kana","@value":"トウホク ニホンコ イナニワダケ チイキ ノ カザンガン ノ Sr Nd Pb ドウイタイ ソセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525709568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北部フォッサマグナに産する後期新生代火山岩のSr-Nd 同位体組成からみた 2 つのソースマントルの分布"},{"@language":"en","@value":"The distributions of two mantle sources based on the Sr-Nd isotopic compositions of late Cenozoic volcanic rocks from the northern Fossa Magna, central Japan"},{"@language":"ja-Kana","@value":"ホクブ フォッサマグナ ニ サンスル コウキ シンセイダイ カザンガン ノ Sr-Nd ドウイタイ ソセイ カラ ミタ 2ツ ノ ソースマントル ノ ブンプ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546056320","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrogenesis of the tholeiitic basalt, calc-alkaline basaltic andesite and high magnesian andesite lava succession of the Oligo-Miocene Anamizu Formation in northeastern Noto Peninsula, central Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390024334626964992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北日本弧火山フロント，福島市南西部に分布する鮮新統～更新統「笹森山火山岩類」の地質学的・岩石学的研究"},{"@language":"en","@value":"Geological and petrological study of “Sasamoriyama Volcanic Rocks” from Pliocene to Pleistocene around the south-western part of Fukushima city in the volcanic front of Northeast Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502126336","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of H2O concentration in primary arc magmas: constraints from melting experiments and analyses of melt inclusions"},{"@language":"ja","@value":"島弧における初生マグマの含水量の推定：実験岩石学とメルト包有物分析からの制約"},{"@language":"ja-Kana","@value":"トウコ ニ オケル ショセイ マグマ ノ ガン スイリョウ ノ スイテイ ジッケン ガンセキガク ト メルト ホウユウブツ ブンセキ カラ ノ セイヤク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681522798976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Operation of subduction factory and production of andesite"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238094102528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-K tholeiitic volcanic rocks of Yoneyama Formation from the northern Fossa Magna, central Japan: Derivative from high water content magma"},{"@language":"ja","@value":"高含水量マグマに由来する高K系列の米山層ソレアイト系列火山岩"},{"@language":"ja-Kana","@value":"コウガン スイリョウ マグマ ニ ユライ スル コウK ケイレツ ノ ヨネヤマソウ ソレアイト ケイレツ カザンガン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417163388800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water content in arc basaltic magma in the Northeast Japan and Izu arcs : an estimate from Ca/Na partitioning between plagioclase and melt"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0024-4937(88)90022-9"},{"@type":"OPENAIRE","@value":"doi_dedup___::02991775d599f0ea7a6a3b21e672a8b8"},{"@type":"CROSSREF","@value":"10.2465/jmps.97.85_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.34.35_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.180602_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1029/2007jb005121_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1144/sp385.15_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/ganko.91.321_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.35.78_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.110131a_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.250714_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1093/petrology/egs065_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/jmps.101.145_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1111/sed.12629_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-127_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1093/petrology/egad009_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2019.105362_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.37.15_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"},{"@type":"CROSSREF","@value":"10.2465/gkk.150701_references_DOI_6WvY2Zo4QyQf7Y5DBR7k8RfzgmF"}]}