Podrobnosti záznamu

Název
    Tectono-metamorphic history recorded in garnet porphyroblasts: insights from thermodynamic modelling and electron backscatter diffraction analysis of inclusion trails
Autor
    Chopin, F.
    Haloda, Jakub
    Lehmann, J.
    Lexa, Ondrej
    Schulmann, Karel
    Skrzypek, Etienne
    Štípská, P.
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Journal of Metamorphic Geology
Svazek/č.
    Č. 29
Strany
    24
Rok
    2011
Výraz tezauru
    electron backscatter diffraction, foliation intersection axes, garnet porphyroblasts, inclusion trails, thermodynamic modelling
Klíčové slovo
    Analysis
    Backscatter
    Diffraction
    Electron
    Garnet
    History
    Inclusion
    Insights
    Modelling
    Porphyroblasts
    Recorded
    Tectono-metamorphic
    Thermodynamic
    Trails
Abstrakt (anglicky)
   In a Barrovian metamorphic sequence, garnetiferous mica schists document a heterogeneously developed superposition of sub-orthogonal fabrics and multiple garnet growth episodes. In the variably deformed domains, four types of garnet porphyroblasts have been defined based on inclusion trail patterns. Modelled garnet zoning in the MnNCKFMASHTO system indicates a prograde evolution from 4-4.5 kbar and 490-510 °C to 5-6 kbar and 520-550 °C in the earliest subhorizontal fabric progressing towards 6.5-7.5 kbar and 560-590 °C in the subsequent subvertical foliation. This fabric is heterogeneously deformed into a shallow-dipping retrograde foliation associated with garnet resorption. In situ electron backscatter diffraction measurements of ilmenite inclusions in individual garnet grains yield precise data on included planar and linear elements. Consistent orientations of internal foliations, lineations and foliation intersection axis sets indicate a superposition of three sub-orthogonal foliat
   ion systems. Weak variations of internal records with increasing intensity of deformation suggest that a moderate buckling stage occurred, but apparent lack of porphyroblast rotation is interpreted as a result of dominant passive flow. Coupling the orientation of internal fabric sets with P-T estimates is used to complement the tectono-metamorphic evolution of the thickened crust. We demonstrate that garnet porphyroblasts preserve features which reflect large-scale tectonic processes in orogens.
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
    R
Datum importu
    15. 10. 2014