On the Move: 2023 Observations on Real Time Graben Formation, Grindavík, Iceland

被引:7
作者
De Pascale, Gregory P. [1 ]
Fischer, Tomas J. [2 ]
Moreland, William Michael [3 ]
Geirsson, Halldor [4 ]
Hrubcova, Pavla [5 ]
Drouin, Vincent [6 ]
Forester, Danielle [3 ]
Payet--Clerc, Meline [3 ,7 ]
da Silveira, Diana Brum [3 ]
Vlcek, Josef [2 ]
Ofeigsson, Benedikt G. [6 ]
Hoskuldsson, Armann [3 ]
Torfadottir, Helga Kristin [3 ]
Valdimarsdottir, Iounn Kara [3 ]
Blondal, Birta Dis Jonsdottir [3 ]
Jonsdottir, Ingibjorg [3 ]
Jonsson, Sigurjon [8 ]
Thordarson, Thor [3 ]
机构
[1] Univ Iceland, Inst Earth Sci, Fac Earth Sci, Reykjavik, Iceland
[2] Charles Univ Prague, Fac Sci, Prague, Czech Republic
[3] Univ Iceland, Fac Earth Sci, Reykjavik, Iceland
[4] Univ Iceland, Inst Earth Sci, Reykjavik, Iceland
[5] Czech Acad Sci, Inst Geophys, Prague, Czech Republic
[6] Iceland Meteorol Off, Reykjavik, Iceland
[7] Univ Paris Cite, Inst Phys Globe Paris, Paris, France
[8] King Abdullah Univ Sci & Technol KAUST, Phys Sci & Engn Div, Thuwal, Saudi Arabia
关键词
Iceland; graben formation; plate boundary; tectonics; reykjanes peninsula; earthquakes; DIKE INTRUSION; PLATE BOUNDARY; DEFORMATION; SEISMICITY; EARTHQUAKES; VOLCANISM; MECHANICS; SWARM;
D O I
10.1029/2024GL110150
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 Grindav & iacute;k. 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 Grindav & iacute;k from 2021 to 2023, attributed to magma intrusions (i.e., dikes), none of these also formed grabens. Thus, the Grindav & iacute;k grabens shows evidence for tectonic origins. Real-time monitoring of these phenomena provide insight into graben formation on Earth and potentially on other planets.
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页数:10
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