Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...

We analyze envelopes of 233 and 22 $M_{\text L}$0.0 to $M_{\text L}$1.8 earthquakes induced by two geothermal stimulations in the Helsinki, Finland, metropolitan area. We separate source spectra and site terms and determine intrinsic attenuation and the scattering strength of shear waves in the 3 Hz...

Full description

Bibliographic Details
Main Authors: Eulenfeld, Tom, Hillers, Gregor, Vuorinen, Tommi A. T., Wegler, Ulrich
Format: Text
Language:unknown
Published: arXiv 2022
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2207.05545
https://arxiv.org/abs/2207.05545
id ftdatacite:10.48550/arxiv.2207.05545
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2207.05545 2023-06-11T04:11:40+02:00 Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ... Eulenfeld, Tom Hillers, Gregor Vuorinen, Tommi A. T. Wegler, Ulrich 2022 https://dx.doi.org/10.48550/arxiv.2207.05545 https://arxiv.org/abs/2207.05545 unknown arXiv https://dx.doi.org/10.1029/2022jb025162 arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Geophysics physics.geo-ph FOS Physical sciences article-journal Text Article ScholarlyArticle 2022 ftdatacite https://doi.org/10.48550/arxiv.2207.0554510.1029/2022jb025162 2023-05-02T10:14:45Z We analyze envelopes of 233 and 22 $M_{\text L}$0.0 to $M_{\text L}$1.8 earthquakes induced by two geothermal stimulations in the Helsinki, Finland, metropolitan area. We separate source spectra and site terms and determine intrinsic attenuation and the scattering strength of shear waves in the 3 Hz to 200 Hz frequency range using radiative transfer based synthetic envelopes. Displacement spectra yield scaling relations with a general deviation from self-similarity, with a stronger albeit more controversial signal from the weaker 2020 stimulation. The 2020 earthquakes also tend to have a smaller local magnitude compared to 2018 earthquakes with the same moment magnitude. We discuss these connections in the context of fluid effects on rupture speed or medium properties. Site terms demonstrate that the spectral amplification relative to two reference borehole sites is not neutral at the other sensors; largest variations are observed at surface stations at frequencies larger than 30 Hz. Intrinsic attenuation is ... : published in JGR: Solid Earth, v2: published version ... Text Fennoscandian DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geophysics physics.geo-ph
FOS Physical sciences
spellingShingle Geophysics physics.geo-ph
FOS Physical sciences
Eulenfeld, Tom
Hillers, Gregor
Vuorinen, Tommi A. T.
Wegler, Ulrich
Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
topic_facet Geophysics physics.geo-ph
FOS Physical sciences
description We analyze envelopes of 233 and 22 $M_{\text L}$0.0 to $M_{\text L}$1.8 earthquakes induced by two geothermal stimulations in the Helsinki, Finland, metropolitan area. We separate source spectra and site terms and determine intrinsic attenuation and the scattering strength of shear waves in the 3 Hz to 200 Hz frequency range using radiative transfer based synthetic envelopes. Displacement spectra yield scaling relations with a general deviation from self-similarity, with a stronger albeit more controversial signal from the weaker 2020 stimulation. The 2020 earthquakes also tend to have a smaller local magnitude compared to 2018 earthquakes with the same moment magnitude. We discuss these connections in the context of fluid effects on rupture speed or medium properties. Site terms demonstrate that the spectral amplification relative to two reference borehole sites is not neutral at the other sensors; largest variations are observed at surface stations at frequencies larger than 30 Hz. Intrinsic attenuation is ... : published in JGR: Solid Earth, v2: published version ...
format Text
author Eulenfeld, Tom
Hillers, Gregor
Vuorinen, Tommi A. T.
Wegler, Ulrich
author_facet Eulenfeld, Tom
Hillers, Gregor
Vuorinen, Tommi A. T.
Wegler, Ulrich
author_sort Eulenfeld, Tom
title Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
title_short Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
title_full Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
title_fullStr Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
title_full_unstemmed Induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the Fennoscandian Shield ...
title_sort induced earthquake source parameters, attenuation, and site effects from waveform envelopes in the fennoscandian shield ...
publisher arXiv
publishDate 2022
url https://dx.doi.org/10.48550/arxiv.2207.05545
https://arxiv.org/abs/2207.05545
genre Fennoscandian
genre_facet Fennoscandian
op_relation https://dx.doi.org/10.1029/2022jb025162
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.2207.0554510.1029/2022jb025162
_version_ 1768386896104259584