Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica

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

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Main Authors: Ikami, Akira, Kaminuma, Katsutada
Language:English
Published: 1984
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/636/files/KJ00000011321.pdf
id ftnipr:oai:nipr.repo.nii.ac.jp:00000636
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00000636 2024-09-09T19:05:15+00:00 Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica Ikami, Akira Kaminuma, Katsutada 1984-02 application/pdf https://nipr.repo.nii.ac.jp/record/636/files/KJ00000011321.pdf eng eng Memoirs of National Institute of Polar Research. Ser. C, Earth sciences 15 29 35 AA00733470 https://nipr.repo.nii.ac.jp/record/636/files/KJ00000011321.pdf 1984 ftnipr 2024-06-17T04:02:37Z P(論文) A refraction experiment with a 100-kg charge was carried out in the ice sheet in the Prince Olav Coast, East Antarctica by the 21st Japanese Antarctic Research Expedition (JARE-21) in 1980. Prominent Rayleigh waves were clearly recorded in a distance range of 2 to 8 km from the explosion point. The maximum period of Rayleigh waves was 0.7 s with a phase velocity of 1.8 km/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 (1.8 km/s in phase velocity), P- and S-wave velocity structures of ice layers to a depth of 300 to 400 m 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 1.85 km/s for the highest velocity model, 1.7 km/s for the middle and 1.6 km/s for the lowest one, and the observed phase velocity at the period of 0.4s was 1.75 km/s. The velocity structure of P- and 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- and S-wave velocities from 100 to 1000 m in depth range from 3.7 to 4.0 km/s, and from 1.8 to 2.0 km/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 100-kg charge was carried out in the ice sheet in the Prince Olav Coast, East Antarctica by the 21st Japanese Antarctic Research Expedition (JARE-21) in 1980. Prominent Rayleigh waves were clearly recorded in a distance range of 2 to 8 km from the explosion point. The maximum period of Rayleigh waves was 0.7 s with a phase velocity of 1.8 km/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 (1.8 km/s in phase velocity), P- and S-wave velocity structures of ice layers to a depth of 300 to 400 m 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 1.85 km/s for the highest velocity model, 1.7 km/s for the middle and 1.6 km/s for the lowest one, and the observed phase velocity at the period of 0.4s was 1.75 km/s. The velocity structure of P- and 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- and S-wave velocities from 100 to 1000 m in depth range from 3.7 to 4.0 km/s, and from 1.8 to 2.0 km/s. departmental bulletin paper
author Ikami, Akira
Kaminuma, Katsutada
spellingShingle Ikami, Akira
Kaminuma, Katsutada
Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
author_facet Ikami, Akira
Kaminuma, Katsutada
author_sort Ikami, Akira
title Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
title_short Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
title_full Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
title_fullStr Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
title_full_unstemmed Velocity distribution on ice sheet in Prince Olav Coast, East Antarctica
title_sort velocity distribution on ice sheet in prince olav coast, east antarctica
publishDate 1984
url https://nipr.repo.nii.ac.jp/record/636/files/KJ00000011321.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. Ser. C, Earth sciences
15
29
35
AA00733470
https://nipr.repo.nii.ac.jp/record/636/files/KJ00000011321.pdf
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