Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...

Understanding dikes is vital as they serve both as bodies that build the crust and as conduits that feed eruptions, and must be monitored to evaluate volcanic hazard. During the 2014-15 Bárðarbunga rifting event, Iceland, intenseseismicity accompanied the intrusion of a ∼ 50 km lateral dike which cu...

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Bibliographic Details
Main Authors: Woods, J, Winder, T, White, RS, Brandsdóttir, B
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2019
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.33723
https://www.repository.cam.ac.uk/handle/1810/286414
id ftdatacite:10.17863/cam.33723
record_format openpolar
spelling ftdatacite:10.17863/cam.33723 2024-02-04T10:01:26+01:00 Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ... Woods, J Winder, T White, RS Brandsdóttir, B 2019 https://dx.doi.org/10.17863/cam.33723 https://www.repository.cam.ac.uk/handle/1810/286414 en eng Elsevier BV Bardarbunga dike intrusion microseismicity cross-correlation rifting induced earthquakes Article ScholarlyArticle JournalArticle article-journal 2019 ftdatacite https://doi.org/10.17863/cam.33723 2024-01-05T15:45:09Z Understanding dikes is vital as they serve both as bodies that build the crust and as conduits that feed eruptions, and must be monitored to evaluate volcanic hazard. During the 2014-15 Bárðarbunga rifting event, Iceland, intenseseismicity accompanied the intrusion of a ∼ 50 km lateral dike which culminated in a 6 month long eruption. We here present relocations of earthquakes induced by the lateral dike intrusion, using cross-correlated, sub-sample relative travel times. The ∼ 100 m spatial resolution achieved reveals the complexity of the dike propagation pathway and dynamics (jerky, segmented), and allows us to address the precise relationship between the dike and seismicity, with direct implications for hazard monitoring. The spatio-temporal characteristics of the induced seismicity can be directly linked in the first instance to propagation of the tip and opening of the dike, and following this - after dike opening - indicate a relationship with magma pressure changes (i.e. dike inflation/deflation), ... Article in Journal/Newspaper Iceland DataCite Metadata Store (German National Library of Science and Technology) Bardarbunga ENVELOPE(-17.528,-17.528,64.635,64.635) Holuhraun ENVELOPE(-16.831,-16.831,64.852,64.852)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Bardarbunga
dike intrusion
microseismicity
cross-correlation
rifting
induced earthquakes
spellingShingle Bardarbunga
dike intrusion
microseismicity
cross-correlation
rifting
induced earthquakes
Woods, J
Winder, T
White, RS
Brandsdóttir, B
Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
topic_facet Bardarbunga
dike intrusion
microseismicity
cross-correlation
rifting
induced earthquakes
description Understanding dikes is vital as they serve both as bodies that build the crust and as conduits that feed eruptions, and must be monitored to evaluate volcanic hazard. During the 2014-15 Bárðarbunga rifting event, Iceland, intenseseismicity accompanied the intrusion of a ∼ 50 km lateral dike which culminated in a 6 month long eruption. We here present relocations of earthquakes induced by the lateral dike intrusion, using cross-correlated, sub-sample relative travel times. The ∼ 100 m spatial resolution achieved reveals the complexity of the dike propagation pathway and dynamics (jerky, segmented), and allows us to address the precise relationship between the dike and seismicity, with direct implications for hazard monitoring. The spatio-temporal characteristics of the induced seismicity can be directly linked in the first instance to propagation of the tip and opening of the dike, and following this - after dike opening - indicate a relationship with magma pressure changes (i.e. dike inflation/deflation), ...
format Article in Journal/Newspaper
author Woods, J
Winder, T
White, RS
Brandsdóttir, B
author_facet Woods, J
Winder, T
White, RS
Brandsdóttir, B
author_sort Woods, J
title Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
title_short Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
title_full Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
title_fullStr Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
title_full_unstemmed Evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: The 2014–15 Bárðarbunga–Holuhraun rifting event, Iceland ...
title_sort evolution of a lateral dike intrusion revealed by relatively-relocated dike-induced earthquakes: the 2014–15 bárðarbunga–holuhraun rifting event, iceland ...
publisher Elsevier BV
publishDate 2019
url https://dx.doi.org/10.17863/cam.33723
https://www.repository.cam.ac.uk/handle/1810/286414
long_lat ENVELOPE(-17.528,-17.528,64.635,64.635)
ENVELOPE(-16.831,-16.831,64.852,64.852)
geographic Bardarbunga
Holuhraun
geographic_facet Bardarbunga
Holuhraun
genre Iceland
genre_facet Iceland
op_doi https://doi.org/10.17863/cam.33723
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