Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F09%3A00000170" target="_blank" >RIV/00025798:_____/09:00000170 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985530:_____/09:00330111

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)

Popis výsledku v původním jazyce

The Cenozoic Most Basin is the largest preserved sedimentary basin within the Eger Graben (the easternmost part of ECRIS) and is interpreted as a part of an incipient rift system that underwent two distinct phases of extension. The first phase, characterised by NNE-SSW- to N-S-oriented horizontal extension between the end of Eocene and early Miocene, was oblique to the rift axis and caused evolution of a fault system characterised by a number of small en-Echelon-arranged E-W (ENE-WSW) faults. The youngest part of the basin fill indicates accelerated subsidence caused probably by the concentration of displacement at several major bounding faults. Major post-depositional faulting and forced folding were related to a change in the extension vector to an orthogonal position with respect to the rift axis and overprinting of the E-W faults by an NE-SW normal fault system.

Název v anglickém jazyce

Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)

Popis výsledku anglicky

The Cenozoic Most Basin is the largest preserved sedimentary basin within the Eger Graben (the easternmost part of ECRIS) and is interpreted as a part of an incipient rift system that underwent two distinct phases of extension. The first phase, characterised by NNE-SSW- to N-S-oriented horizontal extension between the end of Eocene and early Miocene, was oblique to the rift axis and caused evolution of a fault system characterised by a number of small en-Echelon-arranged E-W (ENE-WSW) faults. The youngest part of the basin fill indicates accelerated subsidence caused probably by the concentration of displacement at several major bounding faults. Major post-depositional faulting and forced folding were related to a change in the extension vector to an orthogonal position with respect to the rift axis and overprinting of the E-W faults by an NE-SW normal fault system.

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

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

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

Název periodika

Basin Research

ISSN

0950-091X

e-ISSN

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Svazek periodika

21

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

26

Strana od-do

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Kód UT WoS článku

000266171900001

EID výsledku v databázi Scopus

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