Component in the Source Mechanism
Abstract A volcanic earthquake with Mw 5:6 occurred beneath the Bárdarbunga caldera in Iceland on 29 September 1996. This earthquake is one of a decade-long sequence ofM 5 events at Bárdarbunga with non-double-couple mechanisms in the Global Centroid Moment Tensor catalog. Fortunately, it was record...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.628.7102 2023-05-15T16:46:41+02:00 Component in the Source Mechanism Hrvoje Tkalčić Douglas S. Dreger Gillian R. Foulger Bruce R. Julian The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.7102 http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.7102 http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf text ftciteseerx 2016-01-08T15:20:44Z Abstract A volcanic earthquake with Mw 5:6 occurred beneath the Bárdarbunga caldera in Iceland on 29 September 1996. This earthquake is one of a decade-long sequence ofM 5 events at Bárdarbunga with non-double-couple mechanisms in the Global Centroid Moment Tensor catalog. Fortunately, it was recorded well by the regional-scale Iceland Hotspot Project seismic experiment. We investigated the event with a complete moment tensor inversion method using regional long-period seismic waveforms and a composite structural model. The moment tensor inversion using data from stations of the Iceland Hotspot Project yields a non-double-couple solution with a 67 % vertically oriented compensated linear vector dipole component, a 32 % double-couple component, and a statistically insignificant (2%) volumetric (isotropic) con-traction. This indicates the absence of a net volumetric component, which is puzzling in the case of a large volcanic earthquake that apparently is not explained by shear slip on a planar fault. A possible volcanic mechanism that can produce an earthquake without a volumetric component involves two offset sources with similar but opposite volume changes. We show that although such a model cannot be ruled out, the circumstances under which it could happen are rare. Text Iceland Unknown |
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Abstract A volcanic earthquake with Mw 5:6 occurred beneath the Bárdarbunga caldera in Iceland on 29 September 1996. This earthquake is one of a decade-long sequence ofM 5 events at Bárdarbunga with non-double-couple mechanisms in the Global Centroid Moment Tensor catalog. Fortunately, it was recorded well by the regional-scale Iceland Hotspot Project seismic experiment. We investigated the event with a complete moment tensor inversion method using regional long-period seismic waveforms and a composite structural model. The moment tensor inversion using data from stations of the Iceland Hotspot Project yields a non-double-couple solution with a 67 % vertically oriented compensated linear vector dipole component, a 32 % double-couple component, and a statistically insignificant (2%) volumetric (isotropic) con-traction. This indicates the absence of a net volumetric component, which is puzzling in the case of a large volcanic earthquake that apparently is not explained by shear slip on a planar fault. A possible volcanic mechanism that can produce an earthquake without a volumetric component involves two offset sources with similar but opposite volume changes. We show that although such a model cannot be ruled out, the circumstances under which it could happen are rare. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
author |
Hrvoje Tkalčić Douglas S. Dreger Gillian R. Foulger Bruce R. Julian |
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Hrvoje Tkalčić Douglas S. Dreger Gillian R. Foulger Bruce R. Julian Component in the Source Mechanism |
author_facet |
Hrvoje Tkalčić Douglas S. Dreger Gillian R. Foulger Bruce R. Julian |
author_sort |
Hrvoje Tkalčić |
title |
Component in the Source Mechanism |
title_short |
Component in the Source Mechanism |
title_full |
Component in the Source Mechanism |
title_fullStr |
Component in the Source Mechanism |
title_full_unstemmed |
Component in the Source Mechanism |
title_sort |
component in the source mechanism |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.7102 http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf |
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Iceland |
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Iceland |
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http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.628.7102 http://rses.anu.edu.au/~hrvoje/Tkalcic_etal_BSSA2009.pdf |
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