Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geothermal area in SW Iceland, exploiting a temporary densification of the seismic network 2018 to 2020. Using a subset of 6,300 high-quality manually picked P- and S-phases, we compute a minimum 1-D mod...
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2022
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Online Access: | https://doi.org/10.3389/feart.2022.969836 https://doaj.org/article/20adb7434da742a597e41c08f0562af8 |
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ftdoajarticles:oai:doaj.org/article:20adb7434da742a597e41c08f0562af8 2023-05-15T16:49:37+02:00 Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland Anne Obermann Sin-Mei Wu Thorbjörg Ágústsdóttir Alejandro Duran Tobias Diehl Pilar Sánchez-Pastor Sigridur Kristjansdóttir Vala Hjörleifsdóttir Stefan Wiemer Gylfi Páll Hersir 2022-12-01T00:00:00Z https://doi.org/10.3389/feart.2022.969836 https://doaj.org/article/20adb7434da742a597e41c08f0562af8 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2022.969836/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2022.969836 https://doaj.org/article/20adb7434da742a597e41c08f0562af8 Frontiers in Earth Science, Vol 10 (2022) induced seismicity geothermal tomographic imaging b-value velocity model Science Q article 2022 ftdoajarticles https://doi.org/10.3389/feart.2022.969836 2022-12-30T19:33:45Z We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geothermal area in SW Iceland, exploiting a temporary densification of the seismic network 2018 to 2020. Using a subset of 6,300 high-quality manually picked P- and S-phases, we compute a minimum 1-D model for the region. Our results suggest that the most consistent and accurate hypocenter locations are derived from a joint inversion of P and S arrival times for the Hengill area. We demonstrate that this minimum 1-D model in combination with SeisComP detection and location algorithms can be used to produce fully-automated yet high-quality earthquake catalogs. Our analysis established that both the induced and natural seismicity in the Hengill area occurs in several distinct, spatially constrained clusters. In production and injection areas, the depth of the clusters is at about 2 km, near the bottom of the production and injection wells. These are most likely triggered by the injection and induced by the production, respectively. Outside of these clusters, the seismicity is generally deeper, with the depth of the deepest seismicity indicating the brittle-ductile transition zone. This zone is encountered at about 4 km near the center of the Hengill volcanic area and deepens with increasing distance from its volcanic center, to about 7 km in the southernmost region. A spatial analysis of b-values shows slightly increased values in areas with numerous injection wells and slightly decreased values in production areas. Three-dimensional crustal imaging of VP, VS, VP/VS shows a SE-NW trending fast velocity that extends, at 1–3 km depth between the extinct Grensdalur volcanic center and the presently active Hengill volcanic center. The fastest velocities are found in the NW corner of the Grensdalur volcanic center coinciding with a gravity high and probably reflecting dense solidified magmatic intrusion(s). This trend coincides with traces of geothermal surface manifestations, a shallow lying low resistivity anomaly and an ... Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Hengill ENVELOPE(-21.306,-21.306,64.078,64.078) Grensdalur ENVELOPE(-21.962,-21.962,65.170,65.170) Frontiers in Earth Science 10 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
induced seismicity geothermal tomographic imaging b-value velocity model Science Q |
spellingShingle |
induced seismicity geothermal tomographic imaging b-value velocity model Science Q Anne Obermann Sin-Mei Wu Thorbjörg Ágústsdóttir Alejandro Duran Tobias Diehl Pilar Sánchez-Pastor Sigridur Kristjansdóttir Vala Hjörleifsdóttir Stefan Wiemer Gylfi Páll Hersir Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
topic_facet |
induced seismicity geothermal tomographic imaging b-value velocity model Science Q |
description |
We image shallow crustal structures and analyze seismicity patterns in the Hengill high-enthalpy geothermal area in SW Iceland, exploiting a temporary densification of the seismic network 2018 to 2020. Using a subset of 6,300 high-quality manually picked P- and S-phases, we compute a minimum 1-D model for the region. Our results suggest that the most consistent and accurate hypocenter locations are derived from a joint inversion of P and S arrival times for the Hengill area. We demonstrate that this minimum 1-D model in combination with SeisComP detection and location algorithms can be used to produce fully-automated yet high-quality earthquake catalogs. Our analysis established that both the induced and natural seismicity in the Hengill area occurs in several distinct, spatially constrained clusters. In production and injection areas, the depth of the clusters is at about 2 km, near the bottom of the production and injection wells. These are most likely triggered by the injection and induced by the production, respectively. Outside of these clusters, the seismicity is generally deeper, with the depth of the deepest seismicity indicating the brittle-ductile transition zone. This zone is encountered at about 4 km near the center of the Hengill volcanic area and deepens with increasing distance from its volcanic center, to about 7 km in the southernmost region. A spatial analysis of b-values shows slightly increased values in areas with numerous injection wells and slightly decreased values in production areas. Three-dimensional crustal imaging of VP, VS, VP/VS shows a SE-NW trending fast velocity that extends, at 1–3 km depth between the extinct Grensdalur volcanic center and the presently active Hengill volcanic center. The fastest velocities are found in the NW corner of the Grensdalur volcanic center coinciding with a gravity high and probably reflecting dense solidified magmatic intrusion(s). This trend coincides with traces of geothermal surface manifestations, a shallow lying low resistivity anomaly and an ... |
format |
Article in Journal/Newspaper |
author |
Anne Obermann Sin-Mei Wu Thorbjörg Ágústsdóttir Alejandro Duran Tobias Diehl Pilar Sánchez-Pastor Sigridur Kristjansdóttir Vala Hjörleifsdóttir Stefan Wiemer Gylfi Páll Hersir |
author_facet |
Anne Obermann Sin-Mei Wu Thorbjörg Ágústsdóttir Alejandro Duran Tobias Diehl Pilar Sánchez-Pastor Sigridur Kristjansdóttir Vala Hjörleifsdóttir Stefan Wiemer Gylfi Páll Hersir |
author_sort |
Anne Obermann |
title |
Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
title_short |
Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
title_full |
Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
title_fullStr |
Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
title_full_unstemmed |
Seismicity and 3-D body-wave velocity models across the Hengill geothermal area, SW Iceland |
title_sort |
seismicity and 3-d body-wave velocity models across the hengill geothermal area, sw iceland |
publisher |
Frontiers Media S.A. |
publishDate |
2022 |
url |
https://doi.org/10.3389/feart.2022.969836 https://doaj.org/article/20adb7434da742a597e41c08f0562af8 |
long_lat |
ENVELOPE(-21.306,-21.306,64.078,64.078) ENVELOPE(-21.962,-21.962,65.170,65.170) |
geographic |
Hengill Grensdalur |
geographic_facet |
Hengill Grensdalur |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Frontiers in Earth Science, Vol 10 (2022) |
op_relation |
https://www.frontiersin.org/articles/10.3389/feart.2022.969836/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2022.969836 https://doaj.org/article/20adb7434da742a597e41c08f0562af8 |
op_doi |
https://doi.org/10.3389/feart.2022.969836 |
container_title |
Frontiers in Earth Science |
container_volume |
10 |
_version_ |
1766039756930547712 |