Podrobnosti záznamu

Název
    Primary magnetic fabric in an ultramafic body (Moldanubian Zone, European Variscides) survives exhumation-related granulite-amphibolite facies metamorphism
Autor
    Chlupápčová, Marta
    Faryad, Shah Wali
    Hrouda, František
    Jeřábek, Petr
    Vitouš, Petr
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Lithos
Svazek/č.
    Roč. 111, č. 1-2
Strany
    17
Rok
    2009
Výraz tezauru
    body
    European
    exhumation-related
    fabric
    facies
    granulite-amphibolite
    magnetic
    metamorphism
    (Moldanubian
    Primary
    survives
    ultramafic
    Variscides)
    Zone,
Klíčové slovo
    Body
    European
    Exhumation-related
    Fabric
    Facies
    Granulite-amphibolite
    Magnetic
    Metamorphism
    Moldanubian
    Primary
    Survives
    Ultramafic
    Variscides
    Zone
Abstrakt (anglicky)
   Serpentinized peridotite-clinopyroxenite, approximately 11 x 5 m in size, enclosed in high-pressure felsic granulite. occurs in a quarry near the village of Bory (Gfohl Unit of the Moldanubian Zone of Western Moravia, Czech Republic). The anisotropy of magnetic susceptibility (AMS) was used to investigate the fabrics of both the ultramafic body and the host granulite. The granulite shows a PT path from above 2 GPa/850-900 degrees C following nearly isothermal decompression to sillimanite stability field with subsequent cooling. Two foliations (S-1-preserved only in isoclinal folds and the dominant S-2 foliation parallel to leucocratic bands) are visible in granulite. Through investigating low-field variation of the AMS, one could resolve the AMS into the field-independent and field-dependent components.
Přispěvatel
    UK Praha, Přírodovědecká fakulta
Kód přispěvatele
    UK, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012