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Geothermal evidence of very low glacial temperatures on a rim of the Fennoscandian ice sheet

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    SYSNO ASEP0100738
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JOstatní články
    TitleGeothermal evidence of very low glacial temperatures on a rim of the Fennoscandian ice sheet
    TitleGeotermické důkazy existence velmi nízkých teplot na okraji skandinávského ledovce během poslední doby ledové
    Author(s) Šafanda, Jan (GFU-E) ORCID, RID
    Szewczyk, J. (PL)
    Majorowicz, J. (CA)
    Source TitleGeophysical Research Letters. - : Wiley - ISSN 0094-8276
    Roč. 31, č. 7 (2004), s. L07211/1-4
    Number of pages4 s.
    Languageeng - English
    CountryUS - United States
    Keywordsgeothermal evidence ; glacial temperatures ; Fennoscandian ice sheet
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    R&D ProjectsGA205/03/0998 GA ČR - Czech Science Foundation (CSF)
    IAA3012005 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    KSK3012103 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z3012916 - GFU-E
    AnnotationThe mean ground temperature as low as -10° C and the existence of more than 500 m thick permafrost during the last glacial are apparent from the analysis of deep borehole temperature profiles in north-eastern Poland. The largest thickness of the permafrost and its survival deep into the Holocene was restricted to a region known for its low terrestrial heat flow
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2005

Number of the records: 1  

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