Magnitude scaling of induced earthquakes
Presented are the results of an earthquake magnitude homogenisation exercise for several datasets of induced earthquakes. The result of this exercise is to show that homogeneous computation of earthquake moment- and local-magnitude is useful in hazard assessment of Enhanced Geothermal Systems (EGSs)...
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ftustrathclyde:oai:strathprints.strath.ac.uk:53398 2024-04-28T08:26:04+00:00 Magnitude scaling of induced earthquakes Edwards, Benjamin Douglas, John 2014-10-31 text https://strathprints.strath.ac.uk/53398/ https://strathprints.strath.ac.uk/53398/1/Edwards_Douglas_Geothermics_2014_Magnitude_scaling_of_induced.pdf https://doi.org/10.1016/j.geothermics.2013.09.012 en eng https://strathprints.strath.ac.uk/53398/1/Edwards_Douglas_Geothermics_2014_Magnitude_scaling_of_induced.pdf Edwards, Benjamin and Douglas, John <https://strathprints.strath.ac.uk/view/author/1027421.html> (2014 <https://strathprints.strath.ac.uk/view/year/2014.html>) Magnitude scaling of induced earthquakes. Geothermics <https://strathprints.strath.ac.uk/view/publications/Geothermics.html>, 52. pp. 132-139. ISSN 0375-6505 cc_by_nc_nd Engineering (General). Civil engineering (General) Article PeerReviewed 2014 ftustrathclyde https://doi.org/10.1016/j.geothermics.2013.09.012 2024-04-10T01:04:04Z Presented are the results of an earthquake magnitude homogenisation exercise for several datasets of induced earthquakes. The result of this exercise is to show that homogeneous computation of earthquake moment- and local-magnitude is useful in hazard assessment of Enhanced Geothermal Systems (EGSs). Data include records from EGSs in Basel (Switzerland), Soultz (France) and Cooper Basin (Australia); natural geothermal fields in Geysers (California) and Hengill (Iceland), and a gas field in Roswinkel (Netherlands). Published catalogue magnitudes are shown to differ widely with respect to Mw, with up to a unit of magnitude difference. We explore the scaling between maximum-amplitude and moment-related scales. We find that given a common magnitude definition for the respective types, the scaling between moment- and local-magnitude of small earthquakes follows a second-order polynomial, consistent with previous studies of natural seismicity. Using both the Southern-California ML scale and a PGV-magnitude scale (Mequiv) determined in this study, we find that the datasets fall into two subsets with well-defined relation to Mw: Basel, Geysers and Hengill in one and Soultz and Roswinkel in another (Cooper Basin data were not considered for this part of the analysis because of the limited bandwidth of the instruments). Mequiv is shown to correlate 1:1 with ML, albeit with region-specific offsets, while the distinct subsets in the Mequiv to MW scaling leads us to conclude that source and/or attenuation properties between the respective regions are different. Article in Journal/Newspaper Iceland University of Strathclyde Glasgow: Strathprints Geothermics 52 132 139 |
institution |
Open Polar |
collection |
University of Strathclyde Glasgow: Strathprints |
op_collection_id |
ftustrathclyde |
language |
English |
topic |
Engineering (General). Civil engineering (General) |
spellingShingle |
Engineering (General). Civil engineering (General) Edwards, Benjamin Douglas, John Magnitude scaling of induced earthquakes |
topic_facet |
Engineering (General). Civil engineering (General) |
description |
Presented are the results of an earthquake magnitude homogenisation exercise for several datasets of induced earthquakes. The result of this exercise is to show that homogeneous computation of earthquake moment- and local-magnitude is useful in hazard assessment of Enhanced Geothermal Systems (EGSs). Data include records from EGSs in Basel (Switzerland), Soultz (France) and Cooper Basin (Australia); natural geothermal fields in Geysers (California) and Hengill (Iceland), and a gas field in Roswinkel (Netherlands). Published catalogue magnitudes are shown to differ widely with respect to Mw, with up to a unit of magnitude difference. We explore the scaling between maximum-amplitude and moment-related scales. We find that given a common magnitude definition for the respective types, the scaling between moment- and local-magnitude of small earthquakes follows a second-order polynomial, consistent with previous studies of natural seismicity. Using both the Southern-California ML scale and a PGV-magnitude scale (Mequiv) determined in this study, we find that the datasets fall into two subsets with well-defined relation to Mw: Basel, Geysers and Hengill in one and Soultz and Roswinkel in another (Cooper Basin data were not considered for this part of the analysis because of the limited bandwidth of the instruments). Mequiv is shown to correlate 1:1 with ML, albeit with region-specific offsets, while the distinct subsets in the Mequiv to MW scaling leads us to conclude that source and/or attenuation properties between the respective regions are different. |
format |
Article in Journal/Newspaper |
author |
Edwards, Benjamin Douglas, John |
author_facet |
Edwards, Benjamin Douglas, John |
author_sort |
Edwards, Benjamin |
title |
Magnitude scaling of induced earthquakes |
title_short |
Magnitude scaling of induced earthquakes |
title_full |
Magnitude scaling of induced earthquakes |
title_fullStr |
Magnitude scaling of induced earthquakes |
title_full_unstemmed |
Magnitude scaling of induced earthquakes |
title_sort |
magnitude scaling of induced earthquakes |
publishDate |
2014 |
url |
https://strathprints.strath.ac.uk/53398/ https://strathprints.strath.ac.uk/53398/1/Edwards_Douglas_Geothermics_2014_Magnitude_scaling_of_induced.pdf https://doi.org/10.1016/j.geothermics.2013.09.012 |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
https://strathprints.strath.ac.uk/53398/1/Edwards_Douglas_Geothermics_2014_Magnitude_scaling_of_induced.pdf Edwards, Benjamin and Douglas, John <https://strathprints.strath.ac.uk/view/author/1027421.html> (2014 <https://strathprints.strath.ac.uk/view/year/2014.html>) Magnitude scaling of induced earthquakes. Geothermics <https://strathprints.strath.ac.uk/view/publications/Geothermics.html>, 52. pp. 132-139. ISSN 0375-6505 |
op_rights |
cc_by_nc_nd |
op_doi |
https://doi.org/10.1016/j.geothermics.2013.09.012 |
container_title |
Geothermics |
container_volume |
52 |
container_start_page |
132 |
op_container_end_page |
139 |
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