Identification and Verification of Geodynamic Risk Zones in the Western Carpathians Using Remote Sensing, Geophysical and GNSS Data

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F24%3APU154987" target="_blank" >RIV/00216305:26110/24:PU154987 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61989100:27350/24:10256106

Výsledek na webu

<a href="https://link.springer.com/article/10.1007/s10712-024-09870-8" target="_blank" >https://link.springer.com/article/10.1007/s10712-024-09870-8</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10712-024-09870-8" target="_blank" >10.1007/s10712-024-09870-8</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Identification and Verification of Geodynamic Risk Zones in the Western Carpathians Using Remote Sensing, Geophysical and GNSS Data

Popis výsledku v původním jazyce

Previous surveys using the remote sensing (RS) method revealed significant structures in the area of the Western Carpathians. It has not yet been possible to verify and explain the results of these surveys, even though all the phenomena are regional in nature and show many morphological features that clearly indicate recent activity and deformations, includ- ing current earthquake foci. The aim of the article was to verify these phenomena and com- pare them with new findings. A method of combining geomorphological data with sat- ellite image analysis and verification using Global Navigation Satellite Systems (GNSS) and geophysics data was used. In this work, results are presented confirming the existence of a previously identified nonlinear structure—the "gravity nappe" in the western part of the Low Tatras, and the largest tectonic system Muráň—Malcov is analyzed in detail. Similar structures and tectonic zones, on a smaller scale, can also be found in other areas of the Carpathians. For example, the gravity structure in the Lesser Carpathians and the Ukrainian flysch Carpathians or the linear boundaries interpreted as tectonic systems—the Myjava-Subtatrans, Hron and Transgemerian tectonic zones. Recent movement trends have been confirmed by newly unified data from EUREF Permanent Network (EPN) stations and GNSS campaigns carried out in the last two decades in the given area. Both types of analyzed structures are directly related to the occurring foci of earthquakes.

Název v anglickém jazyce

Identification and Verification of Geodynamic Risk Zones in the Western Carpathians Using Remote Sensing, Geophysical and GNSS Data

Popis výsledku anglicky

Previous surveys using the remote sensing (RS) method revealed significant structures in the area of the Western Carpathians. It has not yet been possible to verify and explain the results of these surveys, even though all the phenomena are regional in nature and show many morphological features that clearly indicate recent activity and deformations, includ- ing current earthquake foci. The aim of the article was to verify these phenomena and com- pare them with new findings. A method of combining geomorphological data with sat- ellite image analysis and verification using Global Navigation Satellite Systems (GNSS) and geophysics data was used. In this work, results are presented confirming the existence of a previously identified nonlinear structure—the "gravity nappe" in the western part of the Low Tatras, and the largest tectonic system Muráň—Malcov is analyzed in detail. Similar structures and tectonic zones, on a smaller scale, can also be found in other areas of the Carpathians. For example, the gravity structure in the Lesser Carpathians and the Ukrainian flysch Carpathians or the linear boundaries interpreted as tectonic systems—the Myjava-Subtatrans, Hron and Transgemerian tectonic zones. Recent movement trends have been confirmed by newly unified data from EUREF Permanent Network (EPN) stations and GNSS campaigns carried out in the last two decades in the given area. Both types of analyzed structures are directly related to the occurring foci of earthquakes.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Surveys in Geophysics

ISSN

0169-3298

e-ISSN

1573-0956

Svazek periodika

neuveden

Číslo periodika v rámci svazku

9870

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

31

Strana od-do

1-31

Kód UT WoS článku

001380453500001

EID výsledku v databázi Scopus

2-s2.0-85212490646