Mechanisms of large earthquakes along the eastern margin of the Japan sea
Fukao, Y. and Furumoto, M., 1975. Mechanism of large earthquakes along the eastern margin of the Japan Sea. Tectonophysics, 25: 247-266 The source mechanisms of large earthquakes occurring along the eastern margin of the Japan Sea are investigated. The earthquakes studied are those off Oga (May 7, 1...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.456.8841 2023-05-15T18:09:16+02:00 Mechanisms of large earthquakes along the eastern margin of the Japan sea Yoshio Fukao Muneyoshi Furumoto The Pennsylvania State University CiteSeerX Archives 1975 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.8841 http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.8841 http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.pdf text 1975 ftciteseerx 2016-01-08T06:15:25Z Fukao, Y. and Furumoto, M., 1975. Mechanism of large earthquakes along the eastern margin of the Japan Sea. Tectonophysics, 25: 247-266 The source mechanisms of large earthquakes occurring along the eastern margin of the Japan Sea are investigated. The earthquakes studied are those off Oga (May 7, 1964), Sakhalin (Sep. 5, 1971) and Shakotan (Aug. 1, 1940) and, though supplementary, the Niigata (Jun. 16, 1964) earthquake. The focal mechanisms of these four earthquakes are predominantly dip-slip reverse faulting on a plane dipping relatively steeply. The strikes of the fault planes are parallel to the general trend of the eastern margin of the Japan Sea. The parameters for the dislocation are determined on the basis of the long-period surface waves and the tsunami heights at the coasts. The stress drop of 126 bars for the Niigata earthquake is significantly large compared to those for the other three shocks. The smallest is the stress drop of 17 bars for the earthquake off Shakotan. This earthquake was found to be especially interesting in two respects. First, the relative excitation of the short- and long-period seismic waves and the tsunami suggests that the dislocation of 1.1 m took place with an abnormally lon exceptionally large area of 50 X 170 km P duration. Second, the fault plane involves an. This fault plane cuts through the entire thick-ness of the lid on the low-velocity zone developing beneath the Japan Sea. The fault plane may manifest a pre-existing fractured zone by which the Japan Sea lithosphere is separated from the northern Japan arc, as far as the west of Hokkaido is concerned. Text Sakhalin Unknown |
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English |
description |
Fukao, Y. and Furumoto, M., 1975. Mechanism of large earthquakes along the eastern margin of the Japan Sea. Tectonophysics, 25: 247-266 The source mechanisms of large earthquakes occurring along the eastern margin of the Japan Sea are investigated. The earthquakes studied are those off Oga (May 7, 1964), Sakhalin (Sep. 5, 1971) and Shakotan (Aug. 1, 1940) and, though supplementary, the Niigata (Jun. 16, 1964) earthquake. The focal mechanisms of these four earthquakes are predominantly dip-slip reverse faulting on a plane dipping relatively steeply. The strikes of the fault planes are parallel to the general trend of the eastern margin of the Japan Sea. The parameters for the dislocation are determined on the basis of the long-period surface waves and the tsunami heights at the coasts. The stress drop of 126 bars for the Niigata earthquake is significantly large compared to those for the other three shocks. The smallest is the stress drop of 17 bars for the earthquake off Shakotan. This earthquake was found to be especially interesting in two respects. First, the relative excitation of the short- and long-period seismic waves and the tsunami suggests that the dislocation of 1.1 m took place with an abnormally lon exceptionally large area of 50 X 170 km P duration. Second, the fault plane involves an. This fault plane cuts through the entire thick-ness of the lid on the low-velocity zone developing beneath the Japan Sea. The fault plane may manifest a pre-existing fractured zone by which the Japan Sea lithosphere is separated from the northern Japan arc, as far as the west of Hokkaido is concerned. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Yoshio Fukao Muneyoshi Furumoto |
spellingShingle |
Yoshio Fukao Muneyoshi Furumoto Mechanisms of large earthquakes along the eastern margin of the Japan sea |
author_facet |
Yoshio Fukao Muneyoshi Furumoto |
author_sort |
Yoshio Fukao |
title |
Mechanisms of large earthquakes along the eastern margin of the Japan sea |
title_short |
Mechanisms of large earthquakes along the eastern margin of the Japan sea |
title_full |
Mechanisms of large earthquakes along the eastern margin of the Japan sea |
title_fullStr |
Mechanisms of large earthquakes along the eastern margin of the Japan sea |
title_full_unstemmed |
Mechanisms of large earthquakes along the eastern margin of the Japan sea |
title_sort |
mechanisms of large earthquakes along the eastern margin of the japan sea |
publishDate |
1975 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.8841 http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.pdf |
genre |
Sakhalin |
genre_facet |
Sakhalin |
op_source |
http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.456.8841 http://www.openseismo.org/contributors/Lee/MoWorking_Backups/Mo2012_0424backup/MoWorking_OLD2/Paper_Pending/Fukao-Furumoto_Tectonophys1974_v26p247.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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1766181737608511488 |