Podrobnosti záznamu

Název
    Geochemistry of the stratified volcanosedimentary complex in the central part of the České středohoří Mts., North Bohemia
Autor
    Balogh, K.
    Cajz, Vladimír
    Erban, V.
    Ulrych, Jaromír
Jazyk
    anglicky
Typ dokumentu
    článek v odborném periodiku
Zdrojový dokument - seriál
    Krystalinikum
Svazek/č.
    Roč. 27, -
Strany
    s. 27-49
Rok
    2001
Poznámky
    Projekt: IAA3111601, GA AV ČR
    Projekt: T014961 and T029897, Hungarian Science Foundation Projects Nos., HU
    Rozsah: 23 s.
    Výzkumný záměr: CEZ:AV0Z3013912
Předmětová kategorie
    Cenozoic
    České středohoří Mts.
    volcanostratigraphy
Klíčové slovo
    Bohemia
    Central
    Complex
    České
    Geochemistry
    Mts
    North
    Stratified
    Středohoří
    Volcanosedimentary
Abstrakt (anglicky)
   On the basis of a new volcanological model and geochemical investigation in the České středohoří Mts., the following volcanostratigraphic formations were recognized: (i) the Lower Fm. - lavas and volcaniclastics of basanitic character (36-26 Ma; Mg# = 57-76; 87Sr/86Sr = 0.703128 -0.703526 and 143Nd/144Nd = 0.512738-0.512849) corresponding to primitive upper mantle products; (ii) the Upper Fm. - lavas and volcaniclastics of trachybasaltic type (31-25 Ma; Mg# = 41-58 87Sr/86Sr = 0.704428-0.704649 and 143Nd /144Nd = 0.512679-0.512742) representing differentiated and partly crustal-contaminated evolved products; (iii) the Uppermost Fm. - flow(s) of basanite (24 Ma), similar in geochemical characteristics to those of the Lower Fm. Volcaniclastic products of the Lower Fm. (Mg# = 51-69) and the Upper Fm. (Mg# = 45-51) also substantially differ in bulk composition. The volcaniclastics underwent alteration to a different degree, which has significantly changed their geochemical signatures.
   Enrichment and depletion in elements, normalized to the massive rocks of the same formation, are highly variable. However, contents of Ti, Al, Si, Fe and (Mn) are relatively stable and these elements represent typical immobile components, whereas Ca, Na, K and Mg contents are Lower; contents of H2O and CO2 are significantly higher. Trace elements such as Nb, Ta, Zr, Hf, REE and Y seem to behave as immobile, whereas Sr, Cu, Ni, Co, Cr, (Th, U) as mobile. The alteration products are mostly represented by minerals of the smectite and zeolite groups.
Přispěvatel
    AV ČR Brno, Geologický ústav
Kód přispěvatele
    AV ČR, GLÚ
Zdrojový formát
    U
Datum importu
    8. 8. 2012