Podrobnosti záznamu

Název
    Petrology of the oldest polymict conglomerate at the eastern margin of the Rhenohercynian Zone: evidence for initial rifting of the Brunovistulian terrane in Moravia
Autor
    Krmíček, Lukáš
    Přichystal, Antonín
Jazyk
    anglicky
Typ dokumentu
    článek ve sborníku
Zdrojový dokument - monografie
    CzechTec07 - 5th Meeting of the Central European Tectonic Studies Group and 12th Meeting of the Czech tectonic Studies Group, April 11-14, 2007, Teplá, Czech Republic
Strany
    2
Poznámky
    Akce: 2007 ; Teplá
Výraz tezauru
    Bohemian Massif
    granite pebbles
    Hády conglomerate
    Moravo-Silesian Devonian
    tetrad effect
Klíčové slovo
    Brunovistulian
    Conglomerate
    Eastern
    Evidence
    Initial
    Margin
    Moravia
    Oldest
    Petrology
    Polymict
    Rhenohercynian
    Rifting
    Terrane
    Zone
Abstrakt (anglicky)
   Middle Devonian coarse-grained (exotic) polymict conglomerate near Brno (called the Hády conglomerate) has been investigated to determine the provenance area. The results of morphometric, petrographic and geochemical study suggests that pebbles belong to eroded upper levels of the Brno Massif and its crystalline envelope. Sedimentation of polymict conglomerate has been accompanied by explosive rhyolitic volcanism with A-type affinity. The Hády conglomerate represents alluvial sediment which was deposited into a continental extension basin. This can be connected very probably with initial phase of the Brunovistulian rifting. The western part of the Brno Massif had to be intensively eroded in the time of the Hády conglomerate formation.
Přispěvatel
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012