The thin hot plume beneath Iceland
We present the results of a seismological investigation of the frequency-dependent amplitude variations across Iceland using data from the HOTSPOT array currently deployed there. The array is composed of 30 broad-band PASSCAL instruments. We use the parameter t*, de¢ned in the usual manner from spec...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.412.695 2023-05-15T16:47:58+02:00 The thin hot plume beneath Iceland Richard M. Allen Guust Nolet W. Jason Morgan Krist| N Vogfjîrd Bergur H. Bergsson Pa Lmi Erlendsson G. R. Foulger Steinunn Jakobsdo Ttir Bruce R. Julian Matt Pritchard Sturla Ragnarsson Ragnar Stefa Nsson The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.412.695 http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.412.695 http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf text ftciteseerx 2016-01-08T03:25:40Z We present the results of a seismological investigation of the frequency-dependent amplitude variations across Iceland using data from the HOTSPOT array currently deployed there. The array is composed of 30 broad-band PASSCAL instruments. We use the parameter t*, de¢ned in the usual manner from spectral ratios (Halderman & Davis 1991), to compare observed S-wave amplitude variations with those predicted due to both anelastic attenuation and di¡raction e¡ects. Four teleseismic events at a range of azimuths are used to measure t*. A 2-D vertical cylindrical plume model with a Gaussian-shaped velocity anomaly is used to model the variations. That part of t* caused by attenuation was estimated by tracing a ray through IASP91, then superimposing our plume model velocity anomaly and calculating the path integral of 1/oQ. That part of t * caused by di¡raction was estimated using a 2-D ¢nite di¡erence code to generate synthetic seismograms. The same spectral ratio technique used for the data was then used to extract a predicted t*. The t * variations caused by anelastic attenuation are unable to account for the variations we observe, but those caused by di¡raction do. We calculate the t * variations caused by di¡raction for di¡erent plume models and obtain Text Iceland Unknown |
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English |
description |
We present the results of a seismological investigation of the frequency-dependent amplitude variations across Iceland using data from the HOTSPOT array currently deployed there. The array is composed of 30 broad-band PASSCAL instruments. We use the parameter t*, de¢ned in the usual manner from spectral ratios (Halderman & Davis 1991), to compare observed S-wave amplitude variations with those predicted due to both anelastic attenuation and di¡raction e¡ects. Four teleseismic events at a range of azimuths are used to measure t*. A 2-D vertical cylindrical plume model with a Gaussian-shaped velocity anomaly is used to model the variations. That part of t* caused by attenuation was estimated by tracing a ray through IASP91, then superimposing our plume model velocity anomaly and calculating the path integral of 1/oQ. That part of t * caused by di¡raction was estimated using a 2-D ¢nite di¡erence code to generate synthetic seismograms. The same spectral ratio technique used for the data was then used to extract a predicted t*. The t * variations caused by anelastic attenuation are unable to account for the variations we observe, but those caused by di¡raction do. We calculate the t * variations caused by di¡raction for di¡erent plume models and obtain |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Richard M. Allen Guust Nolet W. Jason Morgan Krist| N Vogfjîrd Bergur H. Bergsson Pa Lmi Erlendsson G. R. Foulger Steinunn Jakobsdo Ttir Bruce R. Julian Matt Pritchard Sturla Ragnarsson Ragnar Stefa Nsson |
spellingShingle |
Richard M. Allen Guust Nolet W. Jason Morgan Krist| N Vogfjîrd Bergur H. Bergsson Pa Lmi Erlendsson G. R. Foulger Steinunn Jakobsdo Ttir Bruce R. Julian Matt Pritchard Sturla Ragnarsson Ragnar Stefa Nsson The thin hot plume beneath Iceland |
author_facet |
Richard M. Allen Guust Nolet W. Jason Morgan Krist| N Vogfjîrd Bergur H. Bergsson Pa Lmi Erlendsson G. R. Foulger Steinunn Jakobsdo Ttir Bruce R. Julian Matt Pritchard Sturla Ragnarsson Ragnar Stefa Nsson |
author_sort |
Richard M. Allen |
title |
The thin hot plume beneath Iceland |
title_short |
The thin hot plume beneath Iceland |
title_full |
The thin hot plume beneath Iceland |
title_fullStr |
The thin hot plume beneath Iceland |
title_full_unstemmed |
The thin hot plume beneath Iceland |
title_sort |
thin hot plume beneath iceland |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.412.695 http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.412.695 http://seismo.berkeley.edu/~rallen/pub/1997diffraction/GJI1999paper.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766038070041247744 |