QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves
During the period 1981-1993 five deep seismic sounding profiles were performed in Finland as an international co-operation to study the crustal structure of the Fennoscandian Shield. Apart from P-and S-waves, well developed Rayleigh surface waves (R-waves) with periods of 0.5-1.0 s were recorded fro...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.520.2007 2023-05-15T16:13:01+02:00 QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves M. Grad W. Czuba U. Luosto M. Zuchniak The Pennsylvania State University CiteSeerX Archives 1998 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.2007 http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.2007 http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf Key words Q Rayleigh waves Upper Crust Finland text 1998 ftciteseerx 2016-01-08T10:05:27Z During the period 1981-1993 five deep seismic sounding profiles were performed in Finland as an international co-operation to study the crustal structure of the Fennoscandian Shield. Apart from P-and S-waves, well developed Rayleigh surface waves (R-waves) with periods of 0.5-1.0 s were recorded from all the shot points on profiles SVEKA'81, BALTIC, POLAR, SVEKA'91 and FENNIA. In the seismic record sections, filtered in the frequency band 0.5-2.5 Hz, the R-waves were clearly observed up to distances of about 300 km. Short-period recordings from permanent seismograph stations on Finnish territory were used to study the relationship between the amplitude and charge size of the shot points. Amplitudes of R-waves corrected for charge size were used to study QR quality factor of the rocks below the Earth's surface, especially in the uppermost 4 or 5 kilometres. The quality factor QR varies in the uppermost 1 km on average from 30 for Archean basement in the northern and eastern Finland to 60 for the Proterozoic Svecokarelides in Central and Southern Finland. For depths of 1 to 4 km quality factor QR has larger value for both tectonic units being about 130 and 250, respectively. Text Fennoscandian Unknown |
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Key words Q Rayleigh waves Upper Crust Finland |
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Key words Q Rayleigh waves Upper Crust Finland M. Grad W. Czuba U. Luosto M. Zuchniak QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
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Key words Q Rayleigh waves Upper Crust Finland |
description |
During the period 1981-1993 five deep seismic sounding profiles were performed in Finland as an international co-operation to study the crustal structure of the Fennoscandian Shield. Apart from P-and S-waves, well developed Rayleigh surface waves (R-waves) with periods of 0.5-1.0 s were recorded from all the shot points on profiles SVEKA'81, BALTIC, POLAR, SVEKA'91 and FENNIA. In the seismic record sections, filtered in the frequency band 0.5-2.5 Hz, the R-waves were clearly observed up to distances of about 300 km. Short-period recordings from permanent seismograph stations on Finnish territory were used to study the relationship between the amplitude and charge size of the shot points. Amplitudes of R-waves corrected for charge size were used to study QR quality factor of the rocks below the Earth's surface, especially in the uppermost 4 or 5 kilometres. The quality factor QR varies in the uppermost 1 km on average from 30 for Archean basement in the northern and eastern Finland to 60 for the Proterozoic Svecokarelides in Central and Southern Finland. For depths of 1 to 4 km quality factor QR has larger value for both tectonic units being about 130 and 250, respectively. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
M. Grad W. Czuba U. Luosto M. Zuchniak |
author_facet |
M. Grad W. Czuba U. Luosto M. Zuchniak |
author_sort |
M. Grad |
title |
QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
title_short |
QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
title_full |
QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
title_fullStr |
QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
title_full_unstemmed |
QR- Factors in the Crystalline Uppermost Crust in Finland from Rayleigh Surface Waves |
title_sort |
qr- factors in the crystalline uppermost crust in finland from rayleigh surface waves |
publishDate |
1998 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.2007 http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf |
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Fennoscandian |
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Fennoscandian |
op_source |
http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.2007 http://www.geophysica.fi/pdf/geophysica_1998_34_3_115_grad.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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