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

The result's identifiers

  • Result code in 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>

  • Result on the web

    <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>

Alternative languages

  • Result language

    angličtina

  • Original language name

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

  • Original language description

    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.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

  • Continuities

    V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Others

  • Publication year

    2024

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Geologica Carpathica

  • ISSN

    1335-0552

  • e-ISSN

    1336-8052

  • Volume of the periodical

    75

  • Issue of the periodical within the volume

    6

  • Country of publishing house

    SK - SLOVAKIA

  • Number of pages

    12

  • Pages from-to

    375-386

  • UT code for WoS article

    001444337800002

  • EID of the result in the Scopus database