Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...

<p>Intense swarms of microearthquakes have been detected in the rift zone of Central Iceland since the 1970s, but the cause of their clear swarm-like nature remains enigmatic. We use the QuakeMigrate earthquake detection and location software<sup>1</sup> to...

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Main Authors: Winder, Tom, White, Robert S
Format: Conference Object
Language:English
Published: Copernicus GmbH 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.82573
https://www.repository.cam.ac.uk/handle/1810/335141
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spelling ftdatacite:10.17863/cam.82573 2024-02-04T10:01:30+01:00 Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ... Winder, Tom White, Robert S 2022 https://dx.doi.org/10.17863/cam.82573 https://www.repository.cam.ac.uk/handle/1810/335141 en eng Copernicus GmbH restricted All Rights Reserved http://www.rioxx.net/licenses/all-rights-reserved http://purl.org/coar/access_right/c_16ec ScholarlyArticle Presentation Text article-journal 2022 ftdatacite https://doi.org/10.17863/cam.82573 2024-01-05T13:41:45Z <p>Intense swarms of microearthquakes have been detected in the rift zone of Central Iceland since the 1970s, but the cause of their clear swarm-like nature remains enigmatic. We use the QuakeMigrate earthquake detection and location software<sup>1</sup> to produce a highly complete catalogue of microseismicity from 2007-2020, using data from a dense local seismic network. Automatic hypocentre locations have been refined using waveform cross-correlation and double-difference relocation, and tightly constrained focal mechanisms have been obtained by manual analysis of a subset of events.</p><p>The resulting high-resolution earthquake catalogue reveals a network of conjugate strike-slip faults, oriented to accommodate plate-boundary extension. Sharply defined fault planes imaged by the microearthquake hypocentres range from 1-10 km in length, and are found between 1 and 8 km b.s.l., with their orientations closely matching the fault plane ... Conference Object Iceland DataCite Metadata Store (German National Library of Science and Technology)
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collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description <p>Intense swarms of microearthquakes have been detected in the rift zone of Central Iceland since the 1970s, but the cause of their clear swarm-like nature remains enigmatic. We use the QuakeMigrate earthquake detection and location software<sup>1</sup> to produce a highly complete catalogue of microseismicity from 2007-2020, using data from a dense local seismic network. Automatic hypocentre locations have been refined using waveform cross-correlation and double-difference relocation, and tightly constrained focal mechanisms have been obtained by manual analysis of a subset of events.</p><p>The resulting high-resolution earthquake catalogue reveals a network of conjugate strike-slip faults, oriented to accommodate plate-boundary extension. Sharply defined fault planes imaged by the microearthquake hypocentres range from 1-10 km in length, and are found between 1 and 8 km b.s.l., with their orientations closely matching the fault plane ...
format Conference Object
author Winder, Tom
White, Robert S
spellingShingle Winder, Tom
White, Robert S
Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
author_facet Winder, Tom
White, Robert S
author_sort Winder, Tom
title Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
title_short Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
title_full Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
title_fullStr Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
title_full_unstemmed Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? ...
title_sort slowly migrating tectonic microearthquake swarms in the icelandic rift zone: driven by pore-pressure or aseismic slip transients? ...
publisher Copernicus GmbH
publishDate 2022
url https://dx.doi.org/10.17863/cam.82573
https://www.repository.cam.ac.uk/handle/1810/335141
genre Iceland
genre_facet Iceland
op_rights restricted
All Rights Reserved
http://www.rioxx.net/licenses/all-rights-reserved
http://purl.org/coar/access_right/c_16ec
op_doi https://doi.org/10.17863/cam.82573
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