CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS
P(論文) Receiver functions from teleseismic earthquakes recorded with broadband seismographs at Dumont d'Urville Station (66.7°S, 140.0°E; DRV) and Mawson Station (67.6°S, 62.9°E; MAW), East Antarctica, are inverted for shear wave velocity models of the crust and uppermost mantle beneath the reco...
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Language: | English |
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National Institute of Polar Research
1996
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Online Access: | https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 |
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author | カナオ, マサキ クボ, アツキ シブタニ, タクオ KANAO, Masaki KUBO, Atsuki SHIBUTANI, Takuo |
author_facet | カナオ, マサキ クボ, アツキ シブタニ, タクオ KANAO, Masaki KUBO, Atsuki SHIBUTANI, Takuo |
author_sort | カナオ, マサキ |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Receiver functions from teleseismic earthquakes recorded with broadband seismographs at Dumont d'Urville Station (66.7°S, 140.0°E; DRV) and Mawson Station (67.6°S, 62.9°E; MAW), East Antarctica, are inverted for shear wave velocity models of the crust and uppermost mantle beneath the recording stations. The obtained models are compared with the previously obtained ones of Syowa Station (69.0°S, 39.6°E; SYO) to clarify the relationship with regional tectonic history. A crustal velocity model around DRV derived from 18 events indicates a rather sharp Moho at a depth of 38km and somewhat less fluctuation within the crust. It might have originated in the Early Proterozoic metamorphism in Adelie Land. High velocity zones in the upper crust together with low velocity discontinuity of the mid-crust may also have a relation to past tectono-thermal activity. A crustal velocity model around MAW determined by using 20 events has a very sharp Moho at 42km depth that might have developed under high pressure and a thickened crust when a metamorphic event occurred around Mac. Robertson Land in the Late Proterozoic ages. Variation in the crustal velocities at MAW is intermediate among the three stations, which may also have been created by the regional metamorphism. departmental bulletin paper |
genre | Adelie Land Antarc* Antarctica East Antarctica Mac Robertson Land Mac. Robertson Land |
genre_facet | Adelie Land Antarc* Antarctica East Antarctica Mac Robertson Land Mac. Robertson Land |
geographic | East Antarctica Syowa Station Dumont d'Urville Dumont-d'Urville Mawson Station Dumont d'Urville Station Mac. Robertson Land |
geographic_facet | East Antarctica Syowa Station Dumont d'Urville Dumont-d'Urville Mawson Station Dumont d'Urville Station Mac. Robertson Land |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002819 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(140.017,140.017,-66.667,-66.667) ENVELOPE(140.013,140.013,-66.667,-66.667) ENVELOPE(62.874,62.874,-67.603,-67.603) ENVELOPE(140.000,140.000,-66.667,-66.667) ENVELOPE(65.000,65.000,-70.000,-70.000) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002819 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 9 1 15 AA1072335X https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 |
publishDate | 1996 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002819 2025-04-13T14:06:00+00:00 CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS カナオ, マサキ クボ, アツキ シブタニ, タクオ KANAO, Masaki KUBO, Atsuki SHIBUTANI, Takuo 1996-09 application/pdf https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 9 1 15 AA1072335X https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 broadband waveforms teleseismic receiver functions shear wave velocity crustal structure regional metamorphism 1996 ftnipr https://doi.org/10.15094/00002819 2025-03-19T10:19:57Z P(論文) Receiver functions from teleseismic earthquakes recorded with broadband seismographs at Dumont d'Urville Station (66.7°S, 140.0°E; DRV) and Mawson Station (67.6°S, 62.9°E; MAW), East Antarctica, are inverted for shear wave velocity models of the crust and uppermost mantle beneath the recording stations. The obtained models are compared with the previously obtained ones of Syowa Station (69.0°S, 39.6°E; SYO) to clarify the relationship with regional tectonic history. A crustal velocity model around DRV derived from 18 events indicates a rather sharp Moho at a depth of 38km and somewhat less fluctuation within the crust. It might have originated in the Early Proterozoic metamorphism in Adelie Land. High velocity zones in the upper crust together with low velocity discontinuity of the mid-crust may also have a relation to past tectono-thermal activity. A crustal velocity model around MAW determined by using 20 events has a very sharp Moho at 42km depth that might have developed under high pressure and a thickened crust when a metamorphic event occurred around Mac. Robertson Land in the Late Proterozoic ages. Variation in the crustal velocities at MAW is intermediate among the three stations, which may also have been created by the regional metamorphism. departmental bulletin paper Other/Unknown Material Adelie Land Antarc* Antarctica East Antarctica Mac Robertson Land Mac. Robertson Land National Institute of Polar Research Repository, Japan East Antarctica Syowa Station Dumont d'Urville ENVELOPE(140.017,140.017,-66.667,-66.667) Dumont-d'Urville ENVELOPE(140.013,140.013,-66.667,-66.667) Mawson Station ENVELOPE(62.874,62.874,-67.603,-67.603) Dumont d'Urville Station ENVELOPE(140.000,140.000,-66.667,-66.667) Mac. Robertson Land ENVELOPE(65.000,65.000,-70.000,-70.000) |
spellingShingle | broadband waveforms teleseismic receiver functions shear wave velocity crustal structure regional metamorphism カナオ, マサキ クボ, アツキ シブタニ, タクオ KANAO, Masaki KUBO, Atsuki SHIBUTANI, Takuo CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title | CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title_full | CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title_fullStr | CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title_full_unstemmed | CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title_short | CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS |
title_sort | crustal velocity models of shear waves in east antarctica by receiver function inversion of broadband waveforms |
topic | broadband waveforms teleseismic receiver functions shear wave velocity crustal structure regional metamorphism |
topic_facet | broadband waveforms teleseismic receiver functions shear wave velocity crustal structure regional metamorphism |
url | https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 |