2011
Biostratigraphy, sequence stratigraphy and gamma ray spectrometry of the Tournaisian-Visean boundary interval in the Dublin Basin
KALVODA, Jiří; Ondřej BÁBEK; Francois Xavier DEVUYST a George SEVASTOPULOZákladní údaje
Originální název
Biostratigraphy, sequence stratigraphy and gamma ray spectrometry of the Tournaisian-Visean boundary interval in the Dublin Basin
Autoři
KALVODA, Jiří; Ondřej BÁBEK; Francois Xavier DEVUYST a George SEVASTOPULO
Vydání
Bulletin of Geosciences, 2011, 1214-1119
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 1.099
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/11:00050565
Organizační jednotka
Přírodovědecká fakulta
UT WoS
Klíčová slova anglicky
Tournaisian; Viséan; biostratigraphy; sequence stratigraphy; gamma-ray spectrometry
Změněno: 26. 3. 2012 11:25, Ing. Andrea Mikešková
Anotace
V originále
A study of three carbonate and carbonate-siliciclastic sections at the Tournaisian-Visean (Tn-V) boundary in the Dublin Basin (Ireland), has been carried out using high resolution foraminiferal biostratigraphy and gamma-ray spectrometry. The aim was to identify the Tn-V boundary and trace correlatable log patterns in different environmental settings of the Dublin Basin. The foraminiferal fauna in the heterozoan and mixed heterozoan-photozoan (foramderm and bryonoderm extended) late Tournaisian shallow ramp facies and its calciturbidite products is taxonomically impoverished and resembles the similar impoverished foraminiferal associations of western Canada interpreted as reflecting upwelling zones. The increase of photozoan bioclasts which occurs in the latest Tournaisian is accompanied by the entry of important foraminiferal guides of the Tn-V boundary interval. The combination of biostratigraphic and spectral gamma-ray data proved to be a useful tool for the identification of the sequence boundary just below the Tn-V boundary across the different environmental settings of the Dublin Basin. The recognized sea-level fall is correlatable across the London Brabant Massif from western Ireland through to England, South Wales and Belgium.
Návaznosti
| GA205/08/0182, projekt VaV |
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