{"title":"日本北上南带上泥盆统川池组的石鳞藻及其地层意义","authors":"J. Tazawa, I. Niikawa","doi":"10.5575/GEOSOC.2017.0057","DOIUrl":null,"url":null,"abstract":"The Choanji Formation is newly defined as an Upper Devonian (Frasnian ‒ Famennian) sandstone- and shale-dominanted formation, in the Choanji area, South Kitakami Belt, northeastern Japan. The Late Devonian brachiopods, Desquamatia ( Seratrypa ) and Cyrtospirifer occur within the middle and upper parts of the Choanji Formation, respectively. The former is described for the first time in Japan.","PeriodicalId":264556,"journal":{"name":"Journal of the Geological Society of Japan","volume":"118 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-02-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Desquamatia ( Seratrypa ) from the Upper Devonian Choanji Formation in the South Kitakami Belt, Japan, and its stratigraphical significance\",\"authors\":\"J. Tazawa, I. Niikawa\",\"doi\":\"10.5575/GEOSOC.2017.0057\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The Choanji Formation is newly defined as an Upper Devonian (Frasnian ‒ Famennian) sandstone- and shale-dominanted formation, in the Choanji area, South Kitakami Belt, northeastern Japan. The Late Devonian brachiopods, Desquamatia ( Seratrypa ) and Cyrtospirifer occur within the middle and upper parts of the Choanji Formation, respectively. The former is described for the first time in Japan.\",\"PeriodicalId\":264556,\"journal\":{\"name\":\"Journal of the Geological Society of Japan\",\"volume\":\"118 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-02-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Geological Society of Japan\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5575/GEOSOC.2017.0057\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Geological Society of Japan","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5575/GEOSOC.2017.0057","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Desquamatia ( Seratrypa ) from the Upper Devonian Choanji Formation in the South Kitakami Belt, Japan, and its stratigraphical significance
The Choanji Formation is newly defined as an Upper Devonian (Frasnian ‒ Famennian) sandstone- and shale-dominanted formation, in the Choanji area, South Kitakami Belt, northeastern Japan. The Late Devonian brachiopods, Desquamatia ( Seratrypa ) and Cyrtospirifer occur within the middle and upper parts of the Choanji Formation, respectively. The former is described for the first time in Japan.