{"title":"塞尔维亚斯雷姆东部黄土地层与岩性研究","authors":"D. Nenadić, V. Šimić","doi":"10.2298/GABP0566021N","DOIUrl":null,"url":null,"abstract":"Eolian loess sediments in the eastern Srem area, the youngest Pleistocene deposits, occur either as a loess plateau, or as a slope-type of loess, formed on the slopes of the Fru{ka Gora Mountain. Lithological, sedimentological, and mineralogical characteristics of these sediments, which were studied from several com- mon clay deposits and boreholes, demonstrated differences between them and the underlying pre-loess sedi- ments, and supported the stratigraphic division of the Quaternary sediments.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"30 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Stratigraphy and lithology of the loess deposits in eastern Srem, Serbia\",\"authors\":\"D. Nenadić, V. Šimić\",\"doi\":\"10.2298/GABP0566021N\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Eolian loess sediments in the eastern Srem area, the youngest Pleistocene deposits, occur either as a loess plateau, or as a slope-type of loess, formed on the slopes of the Fru{ka Gora Mountain. Lithological, sedimentological, and mineralogical characteristics of these sediments, which were studied from several com- mon clay deposits and boreholes, demonstrated differences between them and the underlying pre-loess sedi- ments, and supported the stratigraphic division of the Quaternary sediments.\",\"PeriodicalId\":263923,\"journal\":{\"name\":\"Geoloski Anali Balkanskog Poluostrva\",\"volume\":\"30 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoloski Anali Balkanskog Poluostrva\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2298/GABP0566021N\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoloski Anali Balkanskog Poluostrva","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2298/GABP0566021N","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Stratigraphy and lithology of the loess deposits in eastern Srem, Serbia
Eolian loess sediments in the eastern Srem area, the youngest Pleistocene deposits, occur either as a loess plateau, or as a slope-type of loess, formed on the slopes of the Fru{ka Gora Mountain. Lithological, sedimentological, and mineralogical characteristics of these sediments, which were studied from several com- mon clay deposits and boreholes, demonstrated differences between them and the underlying pre-loess sedi- ments, and supported the stratigraphic division of the Quaternary sediments.
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