{"@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/1390282681214767232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.5575/geosoc.116.447"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"10814351"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/10814351"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I10814351"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/geosoc/116/8/116_8_447/_pdf"}},{"identifier":{"@type":"NAID","@value":"130000413570"}}],"dc:title":[{"@language":"en","@value":"Chemical composition of whole-rocks samples and volcanic glasses of the Miocene Tamateyama and Sekibutsu Tuffs in the area surrounding the Nara Basin"},{"@language":"ja","@value":"奈良盆地周縁部の玉手山凝灰岩・石仏凝灰岩の火山ガラスおよび全岩の化学組成"},{"@language":"ja-Kana","@value":"ナラ ボンチ シュウエンブ ノ タマテヤマ ギョウカイガン セキブツ ギョウカイガン ノ カザン ガラス オヨビ ゼン ガン ノ カガク ソセイ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"We used XRF and INAA methods to analyze the chemical composition of whole-rock and volcanic glass samples from the Tamateyama and Sekibutsu Tuffs in the area surrounding the Nara Basin. Both tuffs have rhyolitic compositions with SiO<sub>2</sub>=73.6-75.0 wt.%, similar to that of the Muro Pyroclastic Flow Deposits (Muro PFD). The REE patterns of the tuffs are characterized by light REE enrichment, a pronounced negative Eu anomaly, and relatively constant chondrite-normalized middle to heavy REE abundances. These features are similar to those of S-type felsic rocks of the Outer Zone of southwest Japan. Our new petrochemical data provide additional constraints on correlations of the Tamateyama Tuff, Sekibutsu Tuff, and Muro PFD, and indicate that these units were derived from a large felsic igneous body in the Outer Zone of the Kii Peninsula."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801188158976","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60312013"},{"@type":"NRID","@value":"1000060312013"},{"@type":"NRID","@value":"9000414834883"},{"@type":"NRID","@value":"9000258411990"},{"@type":"NRID","@value":"9000016434190"},{"@type":"NRID","@value":"9000414744598"},{"@type":"NRID","@value":"9000257917201"},{"@type":"NRID","@value":"9000259324099"},{"@type":"NRID","@value":"9000001748445"},{"@type":"NRID","@value":"9000017480225"},{"@type":"NRID","@value":"9000411958583"},{"@type":"NRID","@value":"9000257979849"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/hagechabim999"}],"foaf:name":[{"@language":"en","@value":"Shinjoe Hironao"},{"@language":"ja","@value":"新正 裕尚"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Tokyo Keizai University"},{"@language":"ja","@value":"東京経済大学"}]},{"@id":"https://cir.nii.ac.jp/crid/1410571547634648581","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021880729"}],"foaf:name":[{"@language":"en","@value":"Iwano Hideki"},{"@language":"ja","@value":"岩野 英樹"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"（株）京都フィッション・トラック"},{"@language":"en","@value":"Kyoto Fission-Track Co., Ltd."}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204305089409","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000283728122"},{"@type":"NRID","@value":"9000403550400"},{"@type":"NRID","@value":"9000240048529"},{"@type":"NRID","@value":"9000300211826"},{"@type":"NRID","@value":"9000021861351"},{"@type":"NRID","@value":"9000350560829"},{"@type":"NRID","@value":"9000018285759"},{"@type":"NRID","@value":"9000258416918"},{"@type":"NRID","@value":"9000347082128"},{"@type":"NRID","@value":"9000350559470"},{"@type":"NRID","@value":"9000010639411"},{"@type":"NRID","@value":"9000386337022"},{"@type":"NRID","@value":"9000411958582"},{"@type":"NRID","@value":"9000258410864"},{"@type":"NRID","@value":"9000415071771"},{"@type":"NRID","@value":"9000415409583"},{"@type":"NRID","@value":"9000258410862"},{"@type":"NRID","@value":"9000347135760"},{"@type":"NRID","@value":"9000347082136"},{"@type":"NRID","@value":"9000021880734"},{"@type":"NRID","@value":"9000021871138"},{"@type":"NRID","@value":"9000347083133"},{"@type":"NRID","@value":"9000258411186"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/wada.yutaka.nue"}],"foaf:name":[{"@language":"en","@value":"Wada Yutaka"},{"@language":"ja","@value":"和田 穣隆"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"奈良教育大学地学教室"},{"@language":"en","@value":"Department of Earth Sciences, Nara University of Education"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801189294720","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70313046"},{"@type":"NRID","@value":"1000070313046"},{"@type":"NRID","@value":"9000259324137"},{"@type":"NRID","@value":"9000253132401"},{"@type":"NRID","@value":"9000258417977"},{"@type":"NRID","@value":"9000254581552"},{"@type":"NRID","@value":"9000265249747"},{"@type":"NRID","@value":"9000413491123"},{"@type":"NRID","@value":"9000414834884"},{"@type":"NRID","@value":"9000414743301"},{"@type":"NRID","@value":"9000296661818"},{"@type":"NRID","@value":"9000414744596"},{"@type":"NRID","@value":"9000257917202"},{"@type":"NRID","@value":"9000259324100"},{"@type":"NRID","@value":"9000241188935"},{"@type":"NRID","@value":"9000238256993"},{"@type":"NRID","@value":"9000021771501"},{"@type":"NRID","@value":"9000259324079"},{"@type":"NRID","@value":"9000254579358"},{"@type":"NRID","@value":"9000273021477"},{"@type":"NRID","@value":"9000257916806"},{"@type":"NRID","@value":"9000254146854"},{"@type":"NRID","@value":"9000264864578"},{"@type":"NRID","@value":"9000004619974"},{"@type":"NRID","@value":"9000254148365"},{"@type":"NRID","@value":"9000409996001"},{"@type":"NRID","@value":"9000253128854"},{"@type":"NRID","@value":"9000409996006"},{"@type":"NRID","@value":"9000409380786"},{"@type":"NRID","@value":"9000259324115"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0080146"}],"foaf:name":[{"@language":"en","@value":"Orihashi Yuji"},{"@language":"ja","@value":"折橋 裕二"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"東京大学地震研究所"},{"@language":"en","@value":"Earthquake Research Institute, the University of Tokyo"}]},{"@id":"https://cir.nii.ac.jp/crid/1410571547634648577","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021880742"}],"foaf:name":[{"@language":"en","@value":"Sumii Tomoaki"},{"@language":"ja","@value":"角井 朝昭"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Geological Survey of Japan, AIST"},{"@language":"ja","@value":"産業技術研究所地質情報研究部門"}]},{"@id":"https://cir.nii.ac.jp/crid/1410571547634648580","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000021880745"}],"foaf:name":[{"@language":"en","@value":"Danhara Tohru"},{"@language":"ja","@value":"檀原 徹"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"（株）京都フィッション・トラック"},{"@language":"en","@value":"Kyoto Fission-Track Co., Ltd."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167630"},{"@type":"EISSN","@value":"13499963"},{"@type":"CODEN","@value":"CHTZA5"},{"@type":"NDL_BIB_ID","@value":"000000014674"},{"@type":"ISSN","@value":"00167630"},{"@type":"LISSN","@value":"00167630"},{"@type":"NCID","@value":"AN00141768"}],"prism:publicationName":[{"@language":"en","@value":"The Journal of the Geological Society of Japan"},{"@language":"ja","@value":"地質学雑誌"},{"@language":"en","@value":"Jour. Geol. Soc. Japan"},{"@language":"ja","@value":"地質雑"},{"@language":"ja","@value":"地雑"}],"dc:publisher":[{"@language":"en","@value":"The Geological Society of Japan"},{"@language":"ja","@value":"一般社団法人 日本地質学会"}],"prism:publicationDate":"2010","prism:volume":"116","prism:number":"8","prism:startingPage":"447","prism:endingPage":"452"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/10814351"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I10814351"},{"@id":"https://www.jstage.jst.go.jp/article/geosoc/116/8/116_8_447/_pdf"}],"availableAt":"2010","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Tamateyama%20Tuff","dc:title":"Tamateyama Tuff"},{"@id":"https://cir.nii.ac.jp/all?q=Sekibutsu%20Tuff","dc:title":"Sekibutsu Tuff"},{"@id":"https://cir.nii.ac.jp/all?q=Muro%20Pyroclastic%20Flow%20Deposits","dc:title":"Muro Pyroclastic Flow Deposits"},{"@id":"https://cir.nii.ac.jp/all?q=volcanic%20glass","dc:title":"volcanic glass"},{"@id":"https://cir.nii.ac.jp/all?q=trace%20elements","dc:title":"trace elements"},{"@id":"https://cir.nii.ac.jp/all?q=Miocene","dc:title":"Miocene"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360292617911570048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045989758464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic setting of high-Mg andesite magmatism in the SW Japan arc: K-Ar chronology of the Setouchi volcanic belt"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046414863616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SAMPO 90 High resolution interactive gamma-spectrum analysis including automation with macros"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468485191680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of stress in the evolution of large silicic magmatic systems: An example from the Miocene felsic volcanic field at Kii Peninsula, SW Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235305472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fission-track dating of the Setouchi volcanic rocks: An example from the Nijo Group, Kinki district, southwest Japan."},{"@value":"瀬戸内火山岩類のフィッション・トラック年代測定　　近畿地方，二上層群の例"},{"@language":"ja-Kana","@value":"セトウチ カザンガンルイ ノ フィッション トラック ネンダイ ソクテイ キンキ チホウ ニ ジョウソウグン ノ レイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206236850560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Correlation of the Muro Pyroclastic Flow Deposit and the adjacent tuffs in northern Kii Peninsula, southwest Japan, and their source: an approach from mode analysis using refractive index of light minerals"},{"@language":"ja","@value":"紀伊半島北部の室生火砕流堆積物と周辺に分布する凝灰岩の対比およびそれらの給源：軽鉱物屈折率を用いたモード分析によるアプローチ"},{"@language":"ja-Kana","@value":"キイ ハントウ ホクブ ノ ムロウ カサイリュウ タイセキブツ ト シュウヘン ニ ブンプスル ギョウカイガン ノ タイヒ オヨビ ソレラ ノ キュウゲン ケイコウブツ クッセツリツ オ モチイタ モード ブンセキ ニ ヨル アプローチ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526847360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Bulk rock chemistry of the Muro pyroclastic flow deposit: A clue to its source region."},{"@language":"ja","@value":"室生火砕流堆積物の全岩化学組成　　その給源への手掛り"},{"@language":"ja-Kana","@value":"ムロオ カサイリュウ タイセキブツ ノ ゼン ガン カガク ソセイ ソノ キュウゲン エ ノ テガカリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680171720064","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"熊野酸性火成岩類の古地磁気方位"},{"@language":"en","@value":"Paleomagnetic direction of the Kumano Acidic Igneous Rocks, Kii peninsula, Japan."},{"@language":"ja-Kana","@value":"クマノ サンセイ カセイガンルイ ノ コ チジキ ホウイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213561984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simultaneity and similarity of the Muro Pyroclastic Flow Deposit and the Kumano Acidic Rocks in Kii Peninsula, southwest Japan, based on fission track ages and morphological characteristics of zircon"},{"@language":"ja","@value":"ジルコンのフィッション・トラック年代と特徴からみた室生火砕流堆積物と熊野酸性岩類の同時性と類似性"},{"@language":"ja-Kana","@value":"ジルコン ノ フィッション トラック ネンダイ ト トクチョウ カラ ミタ ムロウ カサイリュウ タイセキブツ ト クマノ サンセイガンルイ ノ ドウジセイ ト ルイジセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217190528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Miocene Muro ignimbrite"},{"@language":"ja","@value":"中新世の室生火砕流堆積物"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0035597348"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I10814351"},{"@type":"CROSSREF","@value":"10.5575/geosoc.116.447"},{"@type":"CIA","@value":"130000413570"},{"@type":"OPENAIRE","@value":"doi_dedup___::52ee89b8d151beb3724c09bb61a208ac"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0039_references_DOI_R7FkeoA2EpHQUznXasoMplXEJ36"}]}