Reinterpretation of seismic profiles in the southern part of the Mnichovo Hradiště Basin and south-eastern tip of the Mšeno-Roudnice Basin

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F11%3A10111069" target="_blank" >RIV/00216208:11310/11:10111069 - isvavai.cz</a>

Výsledek na webu

—

DOI - Digital Object Identifier

—

Jazyk výsledku

angličtina

Název v původním jazyce

Reinterpretation of seismic profiles in the southern part of the Mnichovo Hradiště Basin and south-eastern tip of the Mšeno-Roudnice Basin

Popis výsledku v původním jazyce

Results of reinterpretation of seismic measurements in the southern part of the Mnichovo Hradiště Basin and the adjacent south-eastern tip of the Mšeno-Roudnice Basin provide new perspectives for the interpretation of their geological structure and development. Horizontally bedded Upper Cretaceous platform sediments about 400-500 m thick are evidently underlain by Upper Paleozoic and Ordovician deposits as much as 2,200 m and to the N of the area under study even more thick, accompanied by rocks of theUpper Proterozoic basement. The major structures are the Sukorady depression, a half-graben located in the western part of the Mnichovo Hradiště Basin, that is separated from the eastern part of the basin by a zone of the tectonic flexure, and the Luštěnice elevation of apparently WNW-ESE strike. The axis of the Sukorady depression runs approx. NW-SE and its vertical throw increases from 300-400 m, as measured at the Seletice-1 borehole, up to ca 1,800 m in the area between the towns of

Název v anglickém jazyce

Reinterpretation of seismic profiles in the southern part of the Mnichovo Hradiště Basin and south-eastern tip of the Mšeno-Roudnice Basin

Popis výsledku anglicky

Results of reinterpretation of seismic measurements in the southern part of the Mnichovo Hradiště Basin and the adjacent south-eastern tip of the Mšeno-Roudnice Basin provide new perspectives for the interpretation of their geological structure and development. Horizontally bedded Upper Cretaceous platform sediments about 400-500 m thick are evidently underlain by Upper Paleozoic and Ordovician deposits as much as 2,200 m and to the N of the area under study even more thick, accompanied by rocks of theUpper Proterozoic basement. The major structures are the Sukorady depression, a half-graben located in the western part of the Mnichovo Hradiště Basin, that is separated from the eastern part of the basin by a zone of the tectonic flexure, and the Luštěnice elevation of apparently WNW-ESE strike. The axis of the Sukorady depression runs approx. NW-SE and its vertical throw increases from 300-400 m, as measured at the Seletice-1 borehole, up to ca 1,800 m in the area between the towns of

Druh

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

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Folia Musei rerum naturalium Bohemiae occidentalis - Geologica et Paleobiologica

ISSN

1805-2371

e-ISSN

—

Svazek periodika

45

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

60

Strana od-do

1-60

Kód UT WoS článku

—

EID výsledku v databázi Scopus

—