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Structural setting of the České středohoří Mts. volcanic centre, Bohemian Massif, central Europe

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    SYSNO ASEP0050232
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeConference Paper
    TitleStructural setting of the České středohoří Mts. volcanic centre, Bohemian Massif, central Europe
    TitleStrukturní stavba vulkanického centra Českého středohoří
    Author(s) Cajz, Vladimír (GLU-S) RID, SAI, ORCID
    Mrlina, Jan (GFU-E) ORCID, RID
    Adamovič, Jiří (GLU-S) RID, SAI, ORCID
    Mach, Karel (UFCH-W) ORCID, RID
    Chadima, Martin (GLU-S) RID, SAI
    Source TitleLASI II Physical geology of subvolcanic systems: Laccoliths, sills and dykes. - Birmingham : University of Birmingham, Kingston University, 2006 / Thomson K. ; Petford N.
    Pagess. 73-76
    Number of pages4 s.
    ActionPhysical geology of subvolcanic systems: Laccoliths, sills and dykes (LASI) /2./
    Event date01.04.2006-03.04.2006
    VEvent locationBirmingham ; Portree, Isle of Skye
    CountryGB - United Kingdom
    Event typeWRD
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsEger Rift ; České středohoří Mts. ; volcanic centre
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAA3013102 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    IAA300130612 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    AV0Z30120515 - GFU-E (2005-2011)
    AV0Z40400503 - UFCH-W (2005-2011)
    AnnotationThe volcanic centre of the České středohoří Mts. represents area of significant subvolcanic activity. The intrusions of the centre lie intermediate between the most often studied extremes in terms of erosive levels: deep intrusions in the crystalline basement and products of active volcanoes. New geological survey was focused on structural phenomena; besides, a detailed geophysical survey was orientated at hidden subvolcanic bodies. Tectonic setting of the graben interior was identified as blocky one. A computer model of the centre was created down to the level of the crystalline basement, also based on results of detailed tectonic studies.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2007
Number of the records: 1