An evaluation of palaeogeography and palaeoecology in the Most Basin (Czech Republic) and Saxony (Germany) from the late Oligocene to the early Miocene

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10285160" target="_blank" >RIV/00216208:11310/14:10285160 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61388980:_____/14:00428801 RIV/00216208:11410/14:10285160

Výsledek na webu

<a href="http://dx.doi.org/10.1127/0077-7749/2014/0395" target="_blank" >http://dx.doi.org/10.1127/0077-7749/2014/0395</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/0077-7749/2014/0395" target="_blank" >10.1127/0077-7749/2014/0395</a>

Jazyk výsledku

angličtina

Název v původním jazyce

An evaluation of palaeogeography and palaeoecology in the Most Basin (Czech Republic) and Saxony (Germany) from the late Oligocene to the early Miocene

Popis výsledku v původním jazyce

This report concerns sediments in the Most Basin (NW Czech Republic) and coeval Northwest European Tertiary Basin (Germany) connected by a joint trunk river in the time period from the end of the Oligocene to the end of the early Miocene. The re-evaluation of older geochemical and palaeobotanical datasets and newly performed geochemical analyses supported by palaeomagnetic and cyclostratigraphic studies have brought a new insight into the evolution of the studied basins. The relationship between the Most Basin and Saxony sites has been established on the basis of heavy mineral associations of coarse sediments and K, Ti and Al element ratios and cation exchange capacity of finer sediments. The results have allowed us to subdivide the Most Basin evolution into six distinct phases of palaeogeographic evolution related to tectonic and palaeoenvironmental changes. The first palaeogeographic phase in the studied period, from the late Oligocene to the boundary of the Oligocene and Miocene, is

Název v anglickém jazyce

An evaluation of palaeogeography and palaeoecology in the Most Basin (Czech Republic) and Saxony (Germany) from the late Oligocene to the early Miocene

Popis výsledku anglicky

This report concerns sediments in the Most Basin (NW Czech Republic) and coeval Northwest European Tertiary Basin (Germany) connected by a joint trunk river in the time period from the end of the Oligocene to the end of the early Miocene. The re-evaluation of older geochemical and palaeobotanical datasets and newly performed geochemical analyses supported by palaeomagnetic and cyclostratigraphic studies have brought a new insight into the evolution of the studied basins. The relationship between the Most Basin and Saxony sites has been established on the basis of heavy mineral associations of coarse sediments and K, Ti and Al element ratios and cation exchange capacity of finer sediments. The results have allowed us to subdivide the Most Basin evolution into six distinct phases of palaeogeographic evolution related to tectonic and palaeoenvironmental changes. The first palaeogeographic phase in the studied period, from the late Oligocene to the boundary of the Oligocene and Miocene, is

Druh

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

CEP obor

DD - Geochemie

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)<br>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

Neues Jahrbuch für Geologie und Palaontologie - Abhandlungen

ISSN

0077-7749

e-ISSN

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Svazek periodika

272

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

32

Strana od-do

13-45

Kód UT WoS článku

000334585900002

EID výsledku v databázi Scopus

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