Record details

Title
    Magnetostratigraphic investigation of volcanic rock from the Úhošť hill (Doupovské hory Mts.)
Author
    Cajz, Vladimír
    Chadima, Martin
    Pruner, Petr
    Raprich, V.
    Schnabl, Petr
    Šlechta, Stanislav
Conference
    Paleo, Rock and Environmental Magnetism. Castle Meeting (11. : 22.06.2008-28.06.2008 : Bojnice, Slovensko)
Language
    anglicky
Publication type
    abstrakt
Source title - monograph
    Contributions to Geophysics & Geodesy
Pages
    Roč. 38, special issue (2008), s. 125-126
Notes
    Projekt: IAA300130612, GA AV ČR
    Překlad názvu: Magnetostratigrafický výzkum vulkanických hornin na hoře Úhošť (Doupovské hory)
    Rozsah: 2 s. : WWW
    Výzkumný záměr: CEZ:AV0Z30130516
Subject category
    Doupovské hory
    magnetostratigraphy
    Úhošť (Czech Republic)
Keyword
    Doupovské
    Hill
    Hory
    Investigation
    Magnetostratigraphic
    Mts
    Rock
    Úhošť
    Volcanic
Abstract (in english)
   A detailed magnetostratigraphic study was carried out at the locality of Úhošť near Kadaň on the NE margin of the Doupovské hory volcanic complex . Doupovské hory volcanic complex belongs to the Central European alkaline volcanic suite and its genesis is associated with the Eger Graben. The lava flows are consisting of three different rock types: tephrites/basanites, olivine basalts to picrobasalts and basalts s.s. The age of the whole volcanic sequence ranges from 22.09?0.73 to 28.66?1.06 Ma. The mean declination from all localities is 15.8deg and inclination 52.6deg. The parameter alpha95 ranges between 2 and 10 degree. In brief all lava flows has normal polarity. Recently we are measuring succession the 6 lava flows from the west facing hillside of Úhošť that lies just above the measured succession. The preliminary results show also only normal polarity.
Contributor
    AV ČR Brno, Geologický ústav
Contributor code
    AV ČR, GLÚ
Source format
    U
Import date
    8. 8. 2012