Janina Johanna Boesken, C. Zeeden, F. Lehmkuhl, P. Sümegi, N. Klasen
{"title":"Paleoenvironmental analysis of two loess profiles at the Ságvár Lyukas Hill in western Hungary","authors":"Janina Johanna Boesken, C. Zeeden, F. Lehmkuhl, P. Sümegi, N. Klasen","doi":"10.4316/GEOREVIEW.2016.0.0.290","DOIUrl":null,"url":null,"abstract":"Paleoenvironmental investigations are undertaken for two loess profiles at the Sagvar Lyukas Hill in western Hungary. The site is known for its Upper Paleolithic findings (Lengyel, 2008-2009). It is located ca. 12 km south-east of Siofok at Lake Balaton within a loess landscape, which exhibits dominantly northwest-southeast striking valleys. Figure 1 shows a loess map with the location of the site. Granulometric, geochemical, rock magnetic and luminescence analyses were carried out showing weak variations","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"4-5"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.290","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Paleoenvironmental investigations are undertaken for two loess profiles at the Sagvar Lyukas Hill in western Hungary. The site is known for its Upper Paleolithic findings (Lengyel, 2008-2009). It is located ca. 12 km south-east of Siofok at Lake Balaton within a loess landscape, which exhibits dominantly northwest-southeast striking valleys. Figure 1 shows a loess map with the location of the site. Granulometric, geochemical, rock magnetic and luminescence analyses were carried out showing weak variations