2003
Metamorphosed carbonates of Krkonoše Mountains and Paleozoic evolution of Sudetic terranes (NE Bohemia, Czech Republic)
HLADIL, Jindřich, František PATOČKA, Václav KACHLÍK, Rostislav MELICHAR, Martin HUBAČÍK et. al.Základní údaje
Originální název
Metamorphosed carbonates of Krkonoše Mountains and Paleozoic evolution of Sudetic terranes (NE Bohemia, Czech Republic)
Název česky
Metamorfované karbonáty Krkonoš a paleozoický vývoj sudetských teránů (sv. Čechy, Česká republika)
Autoři
HLADIL, Jindřich (203 Česká republika, garant), František PATOČKA (203 Česká republika), Václav KACHLÍK (203 Česká republika), Rostislav MELICHAR (203 Česká republika) a Martin HUBAČÍK (203 Česká republika)
Vydání
Geologica Carpathica, Bratislava, Slovak Academic Press Ltd., 2003, 1335-0552
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Slovensko
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 0.397
Kód RIV
RIV/00216224:14310/03:00010759
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000187610900002
Klíčová slova anglicky
Cambrian; Silurian; Carbonates; Lugicum
Štítky
Změněno: 29. 3. 2010 13:59, doc. RNDr. Rostislav Melichar, Dr.
V originále
The metamorphosed carbonate bodies structurally embedded in the East and South Krkonose Complexes (ESKC - N Bohemian Massif, Krkonose Mountains, Czech Republic) have principally two types of sedimentary precursors. The first precursor corresponds to Early Cambrian dolomitized oolites and microbialites (Dolni Alberice) and provides practically the same fauna and geochemical features on residues as observed in Lusatia (Doberlug-Torgau Syncline). The Cadomian calc-alkaline meta-igneous rock sources, geochemically observed on this Early Cambrian, were also found in the Early Devonian of the Barrandian. The second precursor consists of open-sea calcitic wackestones/packstones and dolomitized packstones/grainstones (Ponikla and Horni Lanov, part) and yields fossil remnants, which are widely comparable with N Gondwanan carbonate sediments of the Bohemian type. The MiddleLate Devonian sedimentary continuation in the ESKC was likely absent (or restricted), and this was preceded by increased geochemical variation of insoluble residues in the marble precursors. Successively diversified compositions of trapped weathering products (regional to inter-regional background sediment, close to Post-Archean Average Australian Sedimentary distribution in REE, with a significant proportion of atmospheric depositions) suggest, that area precursors of the ESKC, Lusatia, Barrandian and Polish Central Sudetes were well separated and expanded to a great extent. The residues from carbonate rocks of the Sudetes correspond to a complex paleotectonic evolution -from Cambrian intracontinental rifting to Devonian arcs. However, there is a trend toward the East and with time toward the Middle Devonian, that Sudetic carbonatic residues indicate a variety of sources posing a wide spectrum of tectonic setting types.
Česky
Nalezené vápence (dolomitizované oolitické vápence, Dolní Albeřice) lze považovat za spodno kambrické.
Návaznosti
MSM 143100004, záměr |
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