Geodetic Signs of the Recent Kinematical and Geodynamical Deformation of the Carpathian Arc

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F19%3APU131432" target="_blank" >RIV/00216305:26110/19:PU131432 - isvavai.cz</a>

Výsledek na webu

<a href="https://iopscience.iop.org/issue/1755-1315/221/1" target="_blank" >https://iopscience.iop.org/issue/1755-1315/221/1</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1088/1755-1315/221/1/012001" target="_blank" >10.1088/1755-1315/221/1/012001</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Geodetic Signs of the Recent Kinematical and Geodynamical Deformation of the Carpathian Arc

Popis výsledku v původním jazyce

Up to now, 4 to 5 models have been presented describing the development of the Carpathian-Pannonian region in terms of subduction processes that took place during the tertiary. All these models are limited to the period between the Paleocene and the Pliocene. None of these, however, explains the Quaternary and Recent phenomena in relation to the postsubduction stage. Several neotectonic models refer to the development of basaltoid volcanism in the south-eastern part of the Pannonian basin. However, the latest geodetic measurements based on GNSS monitoring show a significant kinematics of the internal Carpathian blocks and considerable vertical movement tendencies in the Transylvania, Moldavian and Romanian parts of the platform. The question is the cause of these phenomena and how they are related to earlier processes of subduction. The answer can be found in a comprehensive analysis of geodetic and geophysical data. The main reason for such effort is aspiration to isolate the residual segment of the subduction plate located under the Transylvanian region. The article presents derived geodynamic model based on the combination geodetic with geophysical data, which explain the kinematical tendencies in the eastern and southern Carpathians.

Název v anglickém jazyce

Geodetic Signs of the Recent Kinematical and Geodynamical Deformation of the Carpathian Arc

Popis výsledku anglicky

Up to now, 4 to 5 models have been presented describing the development of the Carpathian-Pannonian region in terms of subduction processes that took place during the tertiary. All these models are limited to the period between the Paleocene and the Pliocene. None of these, however, explains the Quaternary and Recent phenomena in relation to the postsubduction stage. Several neotectonic models refer to the development of basaltoid volcanism in the south-eastern part of the Pannonian basin. However, the latest geodetic measurements based on GNSS monitoring show a significant kinematics of the internal Carpathian blocks and considerable vertical movement tendencies in the Transylvania, Moldavian and Romanian parts of the platform. The question is the cause of these phenomena and how they are related to earlier processes of subduction. The answer can be found in a comprehensive analysis of geodetic and geophysical data. The main reason for such effort is aspiration to isolate the residual segment of the subduction plate located under the Transylvanian region. The article presents derived geodynamic model based on the combination geodetic with geophysical data, which explain the kinematical tendencies in the eastern and southern Carpathians.

Druh

D - Stať ve sborníku

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/LO1408" target="_blank" >LO1408: AdMaS UP - Pokročilé stavební materiály, konstrukce a technologie</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název statě ve sborníku

IOP Conference Series: Earth and Environmental Science

ISBN

978-619-7408-39-3

ISSN

1755-1307

e-ISSN

—

Počet stran výsledku

15

Strana od-do

1-15

Název nakladatele

IOP Publishing Ltd.

Místo vydání

Bristol, Spojené království

Místo konání akce

Prague

Datum konání akce

3. 9. 2018

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

000560708000001