Depositional, burial, thermal, and erosional history along and across the Variscan front, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000048" target="_blank" >RIV/00025798:_____/14:00000048 - 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

Depositional, burial, thermal, and erosional history along and across the Variscan front, Czech Republic

Popis výsledku v původním jazyce

The paper deals with the new approach to basin subdivision, provenance of detrital material, and thermal history. The composition of detrital minerals, such as garnets, provides evidence on the diversity of provenance of the sand bodies and units withinthe original subbasins. The westernmost Andělská hora formation of the Nízký Jeseník (Světlá Greywacke Member) does not have a counterpart in the Drahany Upland. The ?western Culm basin? comprises from S to N the Protivanov and Horní Benešov Fms. with typical polymictic assemblage of translucent heavy minerals and detrital garnets. The eastern Culm basin is subdivided to the lower and upper suite with pyrop-almandine garnets dominating in the latter. The most substantial change within the garnet detritus reflects sudden influx of HT and HP metamorphites into upper suite of the eastern subbasin. The missing Upper Paleozoic units eroded from the original basin and from the later deformed edifice of the Variscan thrust and fold belt were r

Název v anglickém jazyce

Depositional, burial, thermal, and erosional history along and across the Variscan front, Czech Republic

Popis výsledku anglicky

The paper deals with the new approach to basin subdivision, provenance of detrital material, and thermal history. The composition of detrital minerals, such as garnets, provides evidence on the diversity of provenance of the sand bodies and units withinthe original subbasins. The westernmost Andělská hora formation of the Nízký Jeseník (Světlá Greywacke Member) does not have a counterpart in the Drahany Upland. The ?western Culm basin? comprises from S to N the Protivanov and Horní Benešov Fms. with typical polymictic assemblage of translucent heavy minerals and detrital garnets. The eastern Culm basin is subdivided to the lower and upper suite with pyrop-almandine garnets dominating in the latter. The most substantial change within the garnet detritus reflects sudden influx of HT and HP metamorphites into upper suite of the eastern subbasin. The missing Upper Paleozoic units eroded from the original basin and from the later deformed edifice of the Variscan thrust and fold belt were r

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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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 statě ve sborníku

Central European Meeting of Sedimentary Geology, an international conference, Olomouc, Czech Republic, June 9 to 13, 2014, Abstracts

ISBN

978-80-244-4098-9

ISSN

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e-ISSN

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Počet stran výsledku

2

Strana od-do

22-23

Název nakladatele

Palacký University Olomouc

Místo vydání

Olomouc

Místo konání akce

Olomouc

Datum konání akce

1. 1. 2014

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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