Podrobnosti záznamu

Název
    Petrology and geochemistry of the Tertiary alkaline intrusive rocks at Doupov, Doupovské hory Volcanic Complex (NW Bohemian Massif)
Autor
    Erban, Vojtěch
    Holub, František
    Míková, Jitka
    Mlčoch, Bedřich
    Rapprich, Vladislav
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Journal of Geosciences
Svazek/č.
    Roč. 55, č. 3
Strany
    28
Rok
    2010
Výraz tezauru
    alkaline rocks
    Bohemian Massif
    geochemistry
    nephelinolite
    Ohře Graben
    petrology
Klíčové slovo
    Alkaline
    Bohemian
    Complex
    Doupov
    Doupovské
    Geochemistry
    Hory
    Intrusive
    Massif
    NW
    Petrology
    Rocks
    Tertiary
    Volcanic
Abstrakt (anglicky)
   Geochemical variations suggest that the essexitic rocks and sodalite syenitoids do not form a common evolutionary line with nephelinolites. Nephelinolites are isotopically close to the EAR or CMR compositions and interaction of their parental magmas with the continental crust was negligible. Magmatic evolution of nephelinolites was dominated by fractionation of clinopyroxene accompanied at the early stage by olivine and later by titanite, magnetite and apatite. Essexite is isotopically more different though still within the field of mafic lavas from DHVC. Either its parental magma originated in heterogeneous mantle with more distinct lithospheric signature or this magma reacted with the continental crust during its ascent and fractionation. Sodalite monzosyenite displays significantly higher 87Sr/86Sr ratios. The K-Ar ages of intrusive rocks from Doupov are 30-29 Ma.
Přispěvatel
    UK Praha, Přírodovědecká fakulta
Kód přispěvatele
    UK, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012