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  Massive earthquake swarm driven by magmatic intrusion at the Bransfield Strait, Antarctica

Cesca, S., Sugan, M., Rudzinski, Ł., Vajedian, S., Niemz, P., Plank, S., Petersen, G., Deng, Z., Rivalta, E., Vuan, A., Plasencia Linares, M. P., Heimann, S., Dahm, T. (2022): Massive earthquake swarm driven by magmatic intrusion at the Bransfield Strait, Antarctica. - Communications Earth & Environment, 3, 89.
https://doi.org/10.1038/s43247-022-00418-5

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Cesca, Simone1, 2, Author              
Sugan, Monica 2, 3, Author
Rudzinski, Łukasz 2, 3, Author
Vajedian, Sanaz 2, 3, Author
Niemz, P.1, 2, Author              
Plank, Simon 2, 3, Author
Petersen, G.1, 2, Author              
Deng, Z.2, 4, Author              
Rivalta, E.1, 2, Author              
Vuan, Alessandro 2, 3, Author
Plasencia Linares, Milton Percy 2, 3, Author
Heimann, Sebastian 2, 3, Author
Dahm, T.1, 2, Author              
Affiliations:
12.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146029              
2Publikationen aller GIPP-unterstützten Projekte, Deutsches GeoForschungsZentrum, Potsdam, ou_44021              
3External Organizations, ou_persistent22              
41.1 Space Geodetic Techniques, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146025              

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 Abstract: An earthquake swarm affected the Bransfield Strait, Antarctica, a unique rift basin in transition from intra-arc rifting to ocean spreading. The swarm, counting ~85,000 volcano-tectonic earthquakes since August 2020, is located close to the Orca submarine volcano, previously considered inactive. Simultaneously, geodetic data reported up to ~11 cm northwestward displacement over King George Island. We use a broad variety of geophysical data and methods to reveal the complex migration of seismicity, accompanying the intrusion of 0.26–0.56 km3 of magma. Strike-slip earthquakes mark the intrusion at depth, while shallower normal faulting the ~20 km long lateral growth of a dike. Seismicity abruptly decreased after a Mw 6.0 earthquake, suggesting the magmatic dike lost pressure with the slipping of a large fault. A seafloor eruption is likely, but not confirmed by sea surface temperature anomalies. The unrest documents episodic magmatic intrusion in the Bransfield Strait, providing unique insights into active continental rifting.

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 Dates: 20222022
 Publication Status: Finally published
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 Identifiers: DOI: 10.1038/s43247-022-00418-5
GFZPOF: p4 T3 Restless Earth
OATYPE: Gold - DEAL Springer Nature
GFZPOFWEITERE: p4 MESI
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Title: Communications Earth & Environment
Source Genre: Journal, SCI, Scopus, oa
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Pages: - Volume / Issue: 3 Sequence Number: 89 Start / End Page: - Identifier: ISSN: 2662-4435
CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/202009111
Publisher: Springer Nature