Early Palaeozoic Clastic Sediments Found in Boreholes from the SE Surroundings of Brno (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000083" target="_blank" >RIV/00025798:_____/03:00000083 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Early Palaeozoic Clastic Sediments Found in Boreholes from the SE Surroundings of Brno (Czech Republic)

Popis výsledku v původním jazyce

Several boreholes situated in the SE surroundings of Brno penetrated layers of Early Palaeozoic basal clastics (Old Red sandstone) forming part of sedimentary cover of weathered granitoids of the Brno massif. The clastic sediments in several boreholes are palaeontologicaly dated by presence of Acritarcha to Early Cambrian. In the other boreholes an age of the clastics was determined according to their relations to overlying palaeontologicaly dated Early to Middle Devonian limestones. A number of amplesof basal sediments were collected for detailed petrological and geochemical study to differences Cambrian and Devonian clastics. The source area was of the continental arc/active continental margin type, and was dominated by intermediate and acid

Název v anglickém jazyce

Early Palaeozoic Clastic Sediments Found in Boreholes from the SE Surroundings of Brno (Czech Republic)

Popis výsledku anglicky

Several boreholes situated in the SE surroundings of Brno penetrated layers of Early Palaeozoic basal clastics (Old Red sandstone) forming part of sedimentary cover of weathered granitoids of the Brno massif. The clastic sediments in several boreholes are palaeontologicaly dated by presence of Acritarcha to Early Cambrian. In the other boreholes an age of the clastics was determined according to their relations to overlying palaeontologicaly dated Early to Middle Devonian limestones. A number of amplesof basal sediments were collected for detailed petrological and geochemical study to differences Cambrian and Devonian clastics. The source area was of the continental arc/active continental margin type, and was dominated by intermediate and acid

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

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2003

Kód důvěrnosti údajů

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

Název periodika

Geolines

ISSN

1210-9606

e-ISSN

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Svazek periodika

16

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

2

Strana od-do

30-31

Kód UT WoS článku

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EID výsledku v databázi Scopus

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