Podrobnosti záznamu

Název
    Multistage magma emplacement and progressive strain accumulation in the shallow-level Krkonose-Jizera plutonic complex, Bohemian Massif
Autor
    Chlupáčová, M.
    Kachlík, V.
    Sláma, Jiří
    Verner, K.
    Žák, J.
Jazyk
    anglicky
Typ dokumentu
    článek v odborném periodiku
Zdrojový dokument - seriál
    Tectonics
Svazek/č.
    Roč. 32, č. 5
Strany
    s. 1493-1512
Rok
    2013
Poznámky
    Rozsah: 20 s. : P
Předmětová kategorie
    Central-Europe
    fabric development
    Krkonose granite
    magnetic-susceptibility
    Northeastern Brazil
    shrimp zircon
    Sierra-Nevada
    strike-slip tectonics
    SW Poland
    Variscan belt
Klíčové slovo
    Accumulation
    Bohemian
    Complex
    Emplacement
    Krkonose-Jizera
    Magma
    Massif
    Multistage
    Plutonic
    Progressive
    Shallow-level
    Strain
Abstrakt (anglicky)
   Field relationships combined with new U-Pb zircon geochronology suggest that the shallow-level Krkonoše-Jizera plutonic complex, northern Bohemian Massif, was assembled successively from bottom to top, starting with emplacement of the separately evolved S-type Tanvald granite (317.32.1 Ma), followed by at least two voluminous batches of the I-type porphyritic Liberec (319.52.3 Ma) and Jizera (320.13.0 Ma and 319.33.7 Ma) granites. The intrusive sequence was completed by uppermost, minor intrusions of the equigranular Harrachov (315.0 +/- 2.7 Ma) and Krkonoe granites. The I-type granites exhibit an unusually complex pattern of superposed feldspar phenocryst and magnetic fabrics as revealed from the anisotropy of magnetic susceptibility (AMS). The outer Liberec granite preserves margin-parallel foliations and lineations, interpreted to record emplacement-related strain captured by cooling from the pluton floor and walls.
   In contrast, the inner Jizera, Harrachov, and Krkonoe granites were overprinted by synmagmatic strain resulting from dextral movements along regional strike-slip faults cutting the opposite ends of the plutonic complex. Late-stage felsic dikes in the Liberec and Jizera granites reorient from horizontal to vertical (lineation-perpendicular) attitude in response to changing the least principal stress direction, whereas mafic schlieren do not do so, representing only randomly oriented small-scale thermal-mechanical instabilities in the phenocryst framework. In general, this case example challenges the common approach of inferring pluton-wide magma flow from interpolated foliation, lineation, and schlieren patterns. More likely, magmatic fabrics in large plutons record complex temporal succession of superposed strains resulting from diverse processes at multiple scales.
Přispěvatel
    AV ČR Brno, Geologický ústav
Kód přispěvatele
    AV ČR, GLÚ
Zdrojový formát
    U
Datum importu
    23. 10. 2014