0588022 - GFÚ 2025 RIV US eng J - Článek v odborném periodiku
De Pascale, G. P. - Fischer, T. J. - Moreland, W. M. - Geirsson, H. - Hrubcová, Pavla - Drouin, V. - Forester, D. - Payet--Clerc, M. - da Silveira, D. B. - Vlček, J. - Ofeigsson, B. G. - Höskuldsson, Á. - Torfadottir, H. K. - Valdimarsdottir, I. K. - Blondal, B. D. J. - Jonsdottir, I. - Jonsson, S. - Thordarson, T.
On the move: 2023 observations on real time graben formation, Grindavík, Iceland.
Geophysical Research Letters. Roč. 51, č. 14 (2024), č. článku e2024GL110150. ISSN 0094-8276. E-ISSN 1944-8007
Grant CEP: GA ČR(CZ) GA22-10747S; GA TA ČR(CZ) TO01000198
Institucionální podpora: RVO:67985530
Klíčová slova: dike intrusion * plate boundary * volcanism * graben formation * plate boundary * tectonics * earthquakes
Obor OECD: Volcanology
Impakt faktor: 4.6, rok: 2023 ; AIS: 2.03, rok: 2023
Způsob publikování: Open access
Web výsledku:
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GL110150DOI: https://doi.org/10.1029/2024GL110150

Grabens, or valleys formed during extensional tectonic events, are common but rarely observed during formation. In November 2023, inelastic surface deformation formed abruptly along Iceland's plate boundary in Grindavik. We documented graben formation in real-time through satellite mapping (InSAR), seismicity, GNSS data, repeated lidar surveys, and field mapping. Five normal faults and similar to 12 fissures ruptured the surface delineating two grabens separated by a horst, a context not present in other contemporary case studies. The graben normal faults slipped rapidly (over hours) and maximum surface motions coincided with the occurrence of turbulent seismic swarms in both space and time. Although 3 eruptions took place similar to 15 km northeast of Grindavik from 2021 to 2023, attributed to magma intrusions (i.e., dikes), none of these also formed grabens. Thus, the Grindavik grabens shows evidence for tectonic origins. Real-time monitoring of these phenomena provide insight into graben formation on Earth and potentially on other planets.
Trvalý link: https://hdl.handle.net/11104/0355146