Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)

P(論文) A refraction experiment with a 100kg charge was carried out on the ice sheet of the Prince Olav Coast, East Antarctica by the 21st Japanese Antarctic Research Expedition (JARE) in 1980. Prominent Rayleigh waves were clearly recorded in a distance range of 2 to 8km from the explosion point. The...

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Main Authors: Ikami, Akira, Kaminuma, Katsutada
Language:English
Published: 1983
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1463/files/KJ00000012096.pdf
id ftnipr:oai:nipr.repo.nii.ac.jp:00001463
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001463 2024-09-09T19:04:17+00:00 Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract) Ikami, Akira Kaminuma, Katsutada 1983-10 application/pdf https://nipr.repo.nii.ac.jp/record/1463/files/KJ00000012096.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 28 45 AA00733561 https://nipr.repo.nii.ac.jp/record/1463/files/KJ00000012096.pdf 1983 ftnipr 2024-06-17T04:00:39Z P(論文) A refraction experiment with a 100kg charge was carried out on the ice sheet of the Prince Olav Coast, East Antarctica by the 21st Japanese Antarctic Research Expedition (JARE) in 1980. Prominent Rayleigh waves were clearly recorded in a distance range of 2 to 8km from the explosion point. The maximum period of Rayleigh waves was 0.7s with a phase velocity of 1.8km/s. A phase velocity of surface waves is considered to be most sensitive to the P- and S-wave velocity structures of ice layers to a depth of one-fourth of the wave length. Since the longest wave length of Rayleigh waves in the present experiment is estimated to be 1300m for the maximum period of 0.7s (1.8km/s in phase velocity), P-aand S-waves velocity structures of ice layers to a depth of 300 to 400m may be inferred from the dispersion curves. Assuming velocity structures of ice sheet in the Mizuho Plateau based on the previous works of JARE, theoretical dispersion curves were calculated for three different velocity structures and they were compared with the observed ones. For example, the calculated phase velocities at the period of 0.4s were 1.85km/s for the highest velocity model, 1.7km/s for the middle and 1.6km/s for the lowest one and the observed phase velocity at the period of 0.4s was 1.75km/s. The velocity structure of P-aand S-waves in the upper part of ice sheet estimated from observed dispersion curves of Rayleigh waves is three percents higher than those of the averaged one in the Mizuho Plateau. The P-aand S-wave velocities from 100 to 1000m in depth range from 3.7 to 4.0km/s and from 1.8 to 2.0km/s. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica East Antarctica Ice Sheet Memoirs of National Institute of Polar Research Polar Research Prince Olav Coast National Institute of Polar Research Repository, Japan Antarctic East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000) Prince Olav Coast ENVELOPE(41.000,41.000,-69.000,-69.000)
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description P(論文) A refraction experiment with a 100kg charge was carried out on the ice sheet of the Prince Olav Coast, East Antarctica by the 21st Japanese Antarctic Research Expedition (JARE) in 1980. Prominent Rayleigh waves were clearly recorded in a distance range of 2 to 8km from the explosion point. The maximum period of Rayleigh waves was 0.7s with a phase velocity of 1.8km/s. A phase velocity of surface waves is considered to be most sensitive to the P- and S-wave velocity structures of ice layers to a depth of one-fourth of the wave length. Since the longest wave length of Rayleigh waves in the present experiment is estimated to be 1300m for the maximum period of 0.7s (1.8km/s in phase velocity), P-aand S-waves velocity structures of ice layers to a depth of 300 to 400m may be inferred from the dispersion curves. Assuming velocity structures of ice sheet in the Mizuho Plateau based on the previous works of JARE, theoretical dispersion curves were calculated for three different velocity structures and they were compared with the observed ones. For example, the calculated phase velocities at the period of 0.4s were 1.85km/s for the highest velocity model, 1.7km/s for the middle and 1.6km/s for the lowest one and the observed phase velocity at the period of 0.4s was 1.75km/s. The velocity structure of P-aand S-waves in the upper part of ice sheet estimated from observed dispersion curves of Rayleigh waves is three percents higher than those of the averaged one in the Mizuho Plateau. The P-aand S-wave velocities from 100 to 1000m in depth range from 3.7 to 4.0km/s and from 1.8 to 2.0km/s. departmental bulletin paper
author Ikami, Akira
Kaminuma, Katsutada
spellingShingle Ikami, Akira
Kaminuma, Katsutada
Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
author_facet Ikami, Akira
Kaminuma, Katsutada
author_sort Ikami, Akira
title Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
title_short Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
title_full Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
title_fullStr Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
title_full_unstemmed Phase velocity of Rayleigh waves generated by seismic explosions in Prince Olav Coast, East Antarctica (abstract)
title_sort phase velocity of rayleigh waves generated by seismic explosions in prince olav coast, east antarctica (abstract)
publishDate 1983
url https://nipr.repo.nii.ac.jp/record/1463/files/KJ00000012096.pdf
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(40.000,40.000,-73.000,-73.000)
ENVELOPE(41.000,41.000,-69.000,-69.000)
geographic Antarctic
East Antarctica
Mizuho
Mizuho Plateau
Prince Olav Coast
geographic_facet Antarctic
East Antarctica
Mizuho
Mizuho Plateau
Prince Olav Coast
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Memoirs of National Institute of Polar Research
Polar Research
Prince Olav Coast
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Memoirs of National Institute of Polar Research
Polar Research
Prince Olav Coast
op_relation Memoirs of National Institute of Polar Research. Special issue
28
45
AA00733561
https://nipr.repo.nii.ac.jp/record/1463/files/KJ00000012096.pdf
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