{"title":"莫洛地层及其与时间相当的凯氏地层之间 \"不可能 \"的相关性,由强大的沿岸流和偶尔的边缘塌陷所解释","authors":"Sverre Henriksen, Halvor Bunkholt","doi":"10.17850/njg104-1-1","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":0,"journal":{"name":"","volume":" 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2024-04-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Molo Formation and its ‘impossible’ correlation to the time-equivalent Kai Formation explained by strong coastal currents and occasional margin collapse\",\"authors\":\"Sverre Henriksen, Halvor Bunkholt\",\"doi\":\"10.17850/njg104-1-1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":0,\"journal\":{\"name\":\"\",\"volume\":\" 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0,\"publicationDate\":\"2024-04-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.17850/njg104-1-1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.17850/njg104-1-1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The Molo Formation and its ‘impossible’ correlation to the time-equivalent Kai Formation explained by strong coastal currents and occasional margin collapse