Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex

We have determined the three-dimensional P wave velocity structure within the area of the Hengill-Grensdalur central volcano complex, southwest Iceland, from the tomographic inversion of 2409 P wave arrival times recorded by a local earthquake xperiment. The aperture of the 20-element seismic networ...

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Main Authors: D. R. Toomey, G. R. Foulger
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1989
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534
http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.557.534 2023-05-15T16:51:15+02:00 Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex D. R. Toomey G. R. Foulger The Pennsylvania State University CiteSeerX Archives 1989 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534 http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534 http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf text 1989 ftciteseerx 2016-01-08T11:50:57Z We have determined the three-dimensional P wave velocity structure within the area of the Hengill-Grensdalur central volcano complex, southwest Iceland, from the tomographic inversion of 2409 P wave arrival times recorded by a local earthquake xperiment. The aperture of the 20-element seismic network utilized in the inversion permitted imaging ofa 5-km-thick rustal volume underlying a 15 x 14 km 2 area. Within this localized volume are located the underpinnings of the active Hengill volcano and fissure swarm, the extinct Grensdalur volcano, and an active high-temperature g othermal field. It was thus expected that the characteristic length scale of heterogeneity would be of the order of a kilometer. In order to image heterogeneous eismic velocity structure at this scale we paid particular attention to the fidelity of the assumed model parameterization, defined as the degree to which the parameterization can reproduce xpected structural heterogeneity. We also discuss the trade-off between the resolution of model parameters and image fidelity, compare results obtained from different parameterizations t illustrate his trade-off, and present: • synoptic means of assessing image resolution that utilizes the off-diagonal information contained within the resolution matrix. The final tomographic image presented here was determined for a parameterization with fidelity that closely matches the geologic heterogeneity observed on the surface. For this parameterization, the resolution of individual parameters i generally low; however, aquantitative analysis of resolution provides an unambiguous a sessment Text Iceland Unknown Grensdalur ENVELOPE(-21.962,-21.962,65.170,65.170) Hengill ENVELOPE(-21.306,-21.306,64.078,64.078)
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language English
description We have determined the three-dimensional P wave velocity structure within the area of the Hengill-Grensdalur central volcano complex, southwest Iceland, from the tomographic inversion of 2409 P wave arrival times recorded by a local earthquake xperiment. The aperture of the 20-element seismic network utilized in the inversion permitted imaging ofa 5-km-thick rustal volume underlying a 15 x 14 km 2 area. Within this localized volume are located the underpinnings of the active Hengill volcano and fissure swarm, the extinct Grensdalur volcano, and an active high-temperature g othermal field. It was thus expected that the characteristic length scale of heterogeneity would be of the order of a kilometer. In order to image heterogeneous eismic velocity structure at this scale we paid particular attention to the fidelity of the assumed model parameterization, defined as the degree to which the parameterization can reproduce xpected structural heterogeneity. We also discuss the trade-off between the resolution of model parameters and image fidelity, compare results obtained from different parameterizations t illustrate his trade-off, and present: • synoptic means of assessing image resolution that utilizes the off-diagonal information contained within the resolution matrix. The final tomographic image presented here was determined for a parameterization with fidelity that closely matches the geologic heterogeneity observed on the surface. For this parameterization, the resolution of individual parameters i generally low; however, aquantitative analysis of resolution provides an unambiguous a sessment
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author D. R. Toomey
G. R. Foulger
spellingShingle D. R. Toomey
G. R. Foulger
Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
author_facet D. R. Toomey
G. R. Foulger
author_sort D. R. Toomey
title Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
title_short Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
title_full Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
title_fullStr Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
title_full_unstemmed Tomographic inversion of local earthquake data from the Hengill–Grensdalur central volcano complex
title_sort tomographic inversion of local earthquake data from the hengill–grensdalur central volcano complex
publishDate 1989
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534
http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf
long_lat ENVELOPE(-21.962,-21.962,65.170,65.170)
ENVELOPE(-21.306,-21.306,64.078,64.078)
geographic Grensdalur
Hengill
geographic_facet Grensdalur
Hengill
genre Iceland
genre_facet Iceland
op_source http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.534
http://community.dur.ac.uk/g.r.foulger/Offprints/ToomeyFoulger1989.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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