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Palaeomagnetic research of cave sediments in Slovenia in 2007

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    0312844 - GLÚ 2009 SI eng C - Conference Paper (international conference)
    Pruner, Petr - Zupan Hajna, N. - Mihevc, A. - Venhodová, Daniela - Schnabl, Petr - Šlechta, Stanislav - Bosák, Pavel
    Palaeomagnetic research of cave sediments in Slovenia in 2007.
    [Paleomagnetický výzkum jeskynních sedimentů ve Slovinsku v roce 2007.]
    16th International Karstological School Classical Karst : Karst sediments : short scientific papers. Vol. CD ROM 3. Postojna: Institute of Karst Research : ZRC SAZU, 2008 - (Zupan Hajna, N.; Mihevc, A.), s. 1-3
    [International Karstological School "Classical Karst"/16./. Postojna (SI), 16.06.2008-21.06.2008]
    R&D Projects: GA AV ČR IAA300130701
    Grant - others:GA MŠk(CZ) KONTAKT9-06-19; Ministry of Science of Slovenia and Slovenian Research Agency(SI) P6-0119-0618; Ministry of Science of Slovenia and Slovenian Research Agency(SI) P0-119; Ministry of Science of Slovenia and Slovenian Research Agency(SI) J6-6345-0618-04
    Institutional research plan: CEZ:AV0Z30130516
    Source of funding: V - Other public resources
    Keywords : magnetostratigraphy * cave sediments * karst (Slovenia)
    Subject RIV: DE - Earth Magnetism, Geodesy, Geography

    In 2007, sampling of cave fill for palaeomagnetic analysis was performed in several caves in the Classical Karst (SW Slovenia). Standard palaeomagnetic analyses were used (thermal and alternating field demagnetisation, magnetic susceptibility measurements, etc.). Paleomagnetic parameters (inclination, declination) indicate that the respective tectonic block has rotated since the deposition of karst sediments (Tabs. 1 to 3). The rotation differs in different time intervals of the infilling of cave passages and in different karst areas. Repeated sampling in some profiles, especially Divaška jama, Trhlovca, Markov Spodmol, confirmed that only high-resolution approach can ensure reliable results.
    Permanent Link: http://hdl.handle.net/11104/0163801

     
     
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