Tectonic map of the pre-Cenozoic basement of the northern Danube Basin

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F24%3A10259529" target="_blank" >RIV/61989100:27350/24:10259529 - isvavai.cz</a>

Výsledek na webu

<a href="https://geologicacarpathica.com/browse/archive/?journal_article_no=36938" target="_blank" >https://geologicacarpathica.com/browse/archive/?journal_article_no=36938</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.31577/GeolCarp.2024.24" target="_blank" >10.31577/GeolCarp.2024.24</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Tectonic map of the pre-Cenozoic basement of the northern Danube Basin

Popis výsledku v původním jazyce

The Danube Basin is located in the southwest of Slovakia in the northwestern part of the Pannonian Basin System. It consists of Cenozoic deposits, with Miocene sediments comprising the dominant portion in volume. The following paper presents a tectonic map of the pre-Cenozoic basement of the Danube Basin (DB) based on the integration of relevant data from geology, geophysics, biostratigraphy, and tectonics from the past to recently published and archival works. Analysis of boreholes and geophysical data has shown that the western and eastern parts of the DB pre-Cenozoic basement is dominated by Paleozoic crystalline rocks of the Tatric and Veporic nappes, while Mesozoic sediments belonging to the Tatric sedimentary cover, Fatric and Hronic cover nappes are found on the northern margin. The southeastern part of the DB is formed by the rock complexes of the Transdanubian Range Unit. The origin of these Carpathian and Austroalpine tectonic units is the result of Eo-Alpine (Late Cretaceous) tectonic processes. The recent arrangement of the pre-Cenozoic basement was shaped by Neo-Alpine (Miocene) tectonic processes in the extensional/transtension tectonic regime. Tectonic units of Carpathian origin together with the Transdanubian Range Unit can be correlated with the Austroalpine units.

Název v anglickém jazyce

Tectonic map of the pre-Cenozoic basement of the northern Danube Basin

Popis výsledku anglicky

The Danube Basin is located in the southwest of Slovakia in the northwestern part of the Pannonian Basin System. It consists of Cenozoic deposits, with Miocene sediments comprising the dominant portion in volume. The following paper presents a tectonic map of the pre-Cenozoic basement of the Danube Basin (DB) based on the integration of relevant data from geology, geophysics, biostratigraphy, and tectonics from the past to recently published and archival works. Analysis of boreholes and geophysical data has shown that the western and eastern parts of the DB pre-Cenozoic basement is dominated by Paleozoic crystalline rocks of the Tatric and Veporic nappes, while Mesozoic sediments belonging to the Tatric sedimentary cover, Fatric and Hronic cover nappes are found on the northern margin. The southeastern part of the DB is formed by the rock complexes of the Transdanubian Range Unit. The origin of these Carpathian and Austroalpine tectonic units is the result of Eo-Alpine (Late Cretaceous) tectonic processes. The recent arrangement of the pre-Cenozoic basement was shaped by Neo-Alpine (Miocene) tectonic processes in the extensional/transtension tectonic regime. Tectonic units of Carpathian origin together with the Transdanubian Range Unit can be correlated with the Austroalpine units.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10500 - Earth and related environmental sciences

Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Geologica Carpathica

ISSN

1335-0552

e-ISSN

1336-8052

Svazek periodika

75

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

12

Strana od-do

375-386

Kód UT WoS článku

001444337800002

EID výsledku v databázi Scopus

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