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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Main Authors: カナオ, マサキ, クボ, アツキ, シブタニ, タクオ, KANAO, Masaki, KUBO, Atsuki, SHIBUTANI, Takuo
Language:English
Published: National Institute of Polar Research 1996
Subjects:
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
_version_ 1829305479703035904
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