Reconstruction of the unusual Middle Miocene (Badenian) paleoenvironment of the Carpathian Foredeep (Lomnice/Tišnov denudational relict, Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10319589" target="_blank" >RIV/00216208:11310/15:10319589 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.7306/gq.1249" target="_blank" >http://dx.doi.org/10.7306/gq.1249</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.7306/gq.1249" target="_blank" >10.7306/gq.1249</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Reconstruction of the unusual Middle Miocene (Badenian) paleoenvironment of the Carpathian Foredeep (Lomnice/Tišnov denudational relict, Czech Republic)

Popis výsledku v původním jazyce

Multiproxy sedimentological, gamma-spectrometric, foraminiferal, calcareous nannoplankton, and otolith data were used for the reconstruction of the Badenian (Middle Miocene) history of the Moravian part of the Carpathian Foredeep. The study material originated from the new borehole LOM-1, which drilled >20 metres of monotonous clayey siltstones with exceptionally rich and well-preserved microfossil assemblages. Distal parts of the Carpathian Foredeep (a forebulge depozone) are exposed in this succession. Generally, a quiet environment of outer shelf to upper bathyal of monotonous clayey silts was interpreted, which is typical for the proximal parts of a peripheral foreland basin. The section studied can be subdivided into six intervals, confirming thecyclical character of Middle Miocene sedimentation in the Central Paratethys. Interannual oscillations of nutrient content, temperature and/or salinity are interpreted based on the oscillations of geochemical as well as palaeobiological d

Název v anglickém jazyce

Reconstruction of the unusual Middle Miocene (Badenian) paleoenvironment of the Carpathian Foredeep (Lomnice/Tišnov denudational relict, Czech Republic)

Popis výsledku anglicky

Multiproxy sedimentological, gamma-spectrometric, foraminiferal, calcareous nannoplankton, and otolith data were used for the reconstruction of the Badenian (Middle Miocene) history of the Moravian part of the Carpathian Foredeep. The study material originated from the new borehole LOM-1, which drilled >20 metres of monotonous clayey siltstones with exceptionally rich and well-preserved microfossil assemblages. Distal parts of the Carpathian Foredeep (a forebulge depozone) are exposed in this succession. Generally, a quiet environment of outer shelf to upper bathyal of monotonous clayey silts was interpreted, which is typical for the proximal parts of a peripheral foreland basin. The section studied can be subdivided into six intervals, confirming thecyclical character of Middle Miocene sedimentation in the Central Paratethys. Interannual oscillations of nutrient content, temperature and/or salinity are interpreted based on the oscillations of geochemical as well as palaeobiological d

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

2015

Kód důvěrnosti údajů

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

Název periodika

Geological Quarterly

ISSN

1641-7291

e-ISSN

—

Svazek periodika

59

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

25

Strana od-do

654-678

Kód UT WoS článku

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EID výsledku v databázi Scopus

2-s2.0-84952648366