Late Chadian-early Arundian high-resolution biostratigraphy in the Ogmore-by-Sea section (South Wales-Mendip shelf) and the mid-Avonian unconformity

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F14%3A33146111" target="_blank" >RIV/61989592:15310/14:33146111 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/14:00075360

Výsledek na webu

<a href="http://dx.doi.org/10.1144/jgs2013-023" target="_blank" >http://dx.doi.org/10.1144/jgs2013-023</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/jgs2013-023" target="_blank" >10.1144/jgs2013-023</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Late Chadian-early Arundian high-resolution biostratigraphy in the Ogmore-by-Sea section (South Wales-Mendip shelf) and the mid-Avonian unconformity

Popis výsledku v původním jazyce

The study of the foraminiferal fauna in the Ogmore section in south Wales produced a detailed late Chadian-early Arundian biostratigraphy and sequence stratigraphy with a higher resolution than in the Arundian stratotype in Hobbyhorse Bay. The earliest Visean (late Chadian) pedogenic horizon close to the Gully Oolite and Caswell Bay Mudstone boundary (MFZ9) corresponds to the mid-Avonian unconformity. The entry of primitive archaediscids of MFZ10 within the Caswell Bay Mudstone is followed by more advanced archaediscids of MFZ11 at the base of the High Tor Limestone. The mid-Avonian unconformity at the Chadian-Arundian boundary is not confined to the London-Brabant Massif, but is also present in central Europe, the East European Platform, the Urals, west Siberia and probably also in Kuzbass and North America. The global extent of the the mid-Avonian unconformity suggests that it is a consequence of early to mid-Visean glacioeustacy.

Název v anglickém jazyce

Late Chadian-early Arundian high-resolution biostratigraphy in the Ogmore-by-Sea section (South Wales-Mendip shelf) and the mid-Avonian unconformity

Popis výsledku anglicky

The study of the foraminiferal fauna in the Ogmore section in south Wales produced a detailed late Chadian-early Arundian biostratigraphy and sequence stratigraphy with a higher resolution than in the Arundian stratotype in Hobbyhorse Bay. The earliest Visean (late Chadian) pedogenic horizon close to the Gully Oolite and Caswell Bay Mudstone boundary (MFZ9) corresponds to the mid-Avonian unconformity. The entry of primitive archaediscids of MFZ10 within the Caswell Bay Mudstone is followed by more advanced archaediscids of MFZ11 at the base of the High Tor Limestone. The mid-Avonian unconformity at the Chadian-Arundian boundary is not confined to the London-Brabant Massif, but is also present in central Europe, the East European Platform, the Urals, west Siberia and probably also in Kuzbass and North America. The global extent of the the mid-Avonian unconformity suggests that it is a consequence of early to mid-Visean glacioeustacy.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of the Geological Society

ISSN

0016-7649

e-ISSN

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Svazek periodika

171

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

7

Strana od-do

41-47

Kód UT WoS článku

000329924200006

EID výsledku v databázi Scopus

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