Cretaceous stratigraphy of the Silesisan and Subsilesian units in the D48 road cut of the road near Starý Jičín

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F25%3A10169738" target="_blank" >RIV/00025798:_____/25:10169738 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/https://doi.org" target="_blank" >https://doi.org/https://doi.org</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5817/GVMS2025-40985" target="_blank" >10.5817/GVMS2025-40985</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Cretaceous stratigraphy of the Silesisan and Subsilesian units in the D48 road cut of the road near Starý Jičín

Popis výsledku v původním jazyce

A new road cut near Starý Jičín in the external part of the Carpathian Flysch has revealed a tectonic slice with a complex internal structure interpreted as a duplex involving different formations of the Silesian and Subsilesian units. The Silesian Unit includes black pelites of the Hradiště Formation (Barremian-Aptian) and volcanic rocks of the Teschenite Association. The Subsilesian Unit is represented by grey claystones (Cenomanian), clays and paraconglomerates of the Frýdek Formation (Campanian), and claystones with calcareous sandstones of the Frýdlant Formation (Paleocene). Certain Albian and Cenomanian markers species of agglutinated foraminifers were recorded in small quantities already in the Aptian sediments. Hence, the partial-range zones based on deep-sea agglutinated foraminifers, originally proposed by Geroch and Nowak (1984), should be redefined as acme zones.

Název v anglickém jazyce

Cretaceous stratigraphy of the Silesisan and Subsilesian units in the D48 road cut of the road near Starý Jičín

Popis výsledku anglicky

A new road cut near Starý Jičín in the external part of the Carpathian Flysch has revealed a tectonic slice with a complex internal structure interpreted as a duplex involving different formations of the Silesian and Subsilesian units. The Silesian Unit includes black pelites of the Hradiště Formation (Barremian-Aptian) and volcanic rocks of the Teschenite Association. The Subsilesian Unit is represented by grey claystones (Cenomanian), clays and paraconglomerates of the Frýdek Formation (Campanian), and claystones with calcareous sandstones of the Frýdlant Formation (Paleocene). Certain Albian and Cenomanian markers species of agglutinated foraminifers were recorded in small quantities already in the Aptian sediments. Hence, the partial-range zones based on deep-sea agglutinated foraminifers, originally proposed by Geroch and Nowak (1984), should be redefined as acme zones.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

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

Název periodika

Geologické výzkumy na Moravě a ve Slezsku

ISSN

1212-6209

e-ISSN

2336-4378

Svazek periodika

32

Číslo periodika v rámci svazku

1-2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

9

Strana od-do

43-51

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-105025237399