{"@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/1390282679243332608.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.15080/agcjchikyukagaku.22.2_63"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"8295987"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/8295987"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I8295987"}},{"identifier":{"@type":"NAID","@value":"110007089757"}},{"identifier":{"@type":"NAID","@value":"10007644108"}}],"dc:title":[{"@language":"ja","@value":"栃木県葛生町のあど山層から産出したコノドントについて"},{"@language":"en","@value":"The Permian Conodonts in Chert of the Adoyama Formation, Ashio Mountains, Central Japan"},{"@language":"ja-Kana","@value":"トチギケン クズウマチ ノ アドサンソウ カラ サンシュツ シタ コノドント ニ ツイテ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"The Adoyama formation is composed mainly of red, grey, dark grey cherts including sandstone layers. Chert is finely banded in general, and is often intercalated with thin limestone lenses. Just under the Adoyama formation, the Nabeyama formation is conformably underlying, which yields the Permian fusulinids, such as Parafusulina, Pseudofusulina, Schwagerina and Neoschwagerina. Then, the Adoyama formation is undoubtedly the Permian in age. The author collected the samples from only one locality at the base of the Adoyama formation near Kuzu-Machi, Tochigi Pref., Central Japan. Conodonts were obtained by dissolving chert in 5-8% hydrofluoric acid. The author found about 1500 individuals, among which 19 genera and 42 species are described in this paper. Moreover new genus Metapoygnathus is proposed. Characteristic species in this fauna are Gondolella carinata, G. constricta, G. navicula, Gladigondolclla abneptis, G. tethydis and so on. These species have been commonly recognized as the Triassic ones. Polygnathus cf. communis is reported from the Carboniferous, and P. cf mungoensis from the Cretaceous. Both are also included in this fauna. In addition to these, porifera, radiolaria, foraminifera and fish remains are found in the residues of chert."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001204266235008","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000004611266"}],"foaf:name":[{"@language":"ja","@value":"林 信悟"},{"@language":"en","@value":"HAYASHI Shingo"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"前橋支部:群馬県立大間々高等学校"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03666611"},{"@type":"EISSN","@value":"21897212"},{"@type":"NDL_BIB_ID","@value":"000000014627"},{"@type":"ISSN","@value":"03666611"},{"@type":"LISSN","@value":"03666611"},{"@type":"NCID","@value":"AN00141269"}],"prism:publicationName":[{"@language":"ja","@value":"地球科学"},{"@language":"en","@value":"Earth Science (Chikyu Kagaku)"},{"@language":"ja","@value":"地球科学"},{"@language":"en","@value":"Chikyu Kagaku"},{"@language":"ja","@value":"地球科學"}],"dc:publisher":[{"@language":"en","@value":"The Association for the Geological Collaboration in Japan"},{"@language":"ja","@value":"地学団体研究会"}],"prism:publicationDate":"1968","prism:volume":"22","prism:number":"2","prism:startingPage":"63","prism:endingPage":"77"},"url":[{"@id":"http://id.ndl.go.jp/bib/8295987"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I8295987"}],"availableAt":"1968","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001206238336512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Early Jurassic radiolarians from pelitic rocks in the Mino Belt, Nyukawa Village, Gifu Prefecture, central Japan"},{"@value":"岐阜県丹生川村の美濃帯泥質岩より得られた前期ジュラ紀放散虫化石"},{"@language":"ja-Kana","@value":"ギフケン ニュウカワムラ ノ ミノタイ デイシツガン ヨリ エラレタ ゼンキ ジュラキ ホウサンチュウ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288129731968","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A report of Permian, Triassic, and Jurassic radiolarian occurrences from the Ashio terrane in the Hachioji Hills, eastern Gunma Prefecture, central Japan"},{"@language":"ja","@value":"群馬県東部八王子丘陵の足尾テレーンから産出したペルム紀，三畳紀及びジュラ紀放散虫の報告"}]},{"@id":"https://cir.nii.ac.jp/crid/1390008299692243712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"足尾山地のジュラ紀付加体の地質と対比：5 万分の1 地質図幅「桐生及足利」地域の検討"},{"@language":"en","@value":"Geology and correlation of Jurassic accretionary complex in the Ashio Mountains, central Japan: Investigation on the Kiryu and Ashikaga District (Quadrangle series 1:50,000)"},{"@language":"ja-Kana","@value":"アシオ サンチ ノ ジュラキ フカタイ ノ チシツ ト タイヒ : 5マンブン ノ 1 チシツ ズフク 「 キリュウ オヨビ アシカガ 」 チイキ ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214861312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lithostratigraphy, conodont ages, and oceanic plate stratigraphic correlation of deep-water pelagic limestone from Kutajima Island, Kagoshima, southwest Japan"},{"@language":"ja","@value":"鹿児島県久多島の深海遠洋性石灰岩の層序・コノドント化石年代と海洋プレート層序学的比較"},{"@language":"ja-Kana","@value":"カゴシマケン クタジマ ノ シンカイ エンヨウセイ セッカイガン ノ ソウジョ コノドント カセキ ネンダイ ト カイヨウ プレート ソウジョガクテキ ヒカク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390289774666780672","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Radiolarians from Jurassic accretionary complex of the Ashio belt in the Kiryu and Ashikaga District (Quadrangle series 1:50,000), central Japan"},{"@language":"ja","@value":"5 万分の1 地質図幅「桐生及足利」地域の足尾帯ジュラ紀付加体から産出した放散虫"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238083402368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"コノドント生層序による中部三畳系アニシアン遠洋深海層状チャートにおける放散虫化石帯年代の再検討"},{"@language":"en","@value":"Conodont-based age calibration of the Middle Triassic Anisian radiolarian biozones in pelagic deep-sea bedded chert"}]},{"@id":"https://cir.nii.ac.jp/crid/1390571249644546816","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Conodont fossils from the Kiryu and Ashikaga District (Quadrangle series 1:50,000),central Japan with emphasis on the reexamination of “Carboniferous” conodonts from the Ashio Belt"},{"@language":"ja","@value":"5 万分の1 地質図幅「桐生及足利」地域から産出したコノドント化石：足尾テレーンの“石炭紀”コノドントを中心とした再検討"}]},{"@id":"https://cir.nii.ac.jp/crid/1390575451210128512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"巡検案内書：足尾山地南西部「桐生及足利」地域のジュラ紀付加体"},{"@language":"en","@value":"Field excursion guide: Jurassic accretionary complex in the Kiryu and Ashikaga District, southwestern Ashio Mountains, central Japan"},{"@language":"ja-Kana","@value":"ジュンケン アンナイショ : アシオ サンチ ナンセイブ 「 キリュウ オヨビ アシカガ 」 チイキ ノ ジュラキ フカタイ"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2002958497"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I8295987"},{"@type":"CIA","@value":"10007644108"},{"@type":"CIA","@value":"110007089757"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.70.43_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.70.225_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.72.325_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.72.201_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.72.287_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.73.4_143_references_DOI_FglJ9s5tYEEc7S6tpeluD1GphIc"}]}