The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica

P(論文) At Mizuho Station (70°42'S, 44°20'E) velocity profiles of P and S waves down to a depth of 208m were measured on 30 July and 1 August 1983,the waves were generated by hitting an iron block set on the snow surface and traveled waves were detected by geophones set in boreholes. It was...

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Main Authors: Ishizawa, Kenji, Mae, Shinji
Language:English
Published: 1985
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1842/files/KJ00000012474.pdf
https://nipr.repo.nii.ac.jp/records/1842
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author Ishizawa, Kenji
Mae, Shinji
author_facet Ishizawa, Kenji
Mae, Shinji
author_sort Ishizawa, Kenji
collection National Institute of Polar Research Repository, Japan
description P(論文) At Mizuho Station (70°42'S, 44°20'E) velocity profiles of P and S waves down to a depth of 208m were measured on 30 July and 1 August 1983,the waves were generated by hitting an iron block set on the snow surface and traveled waves were detected by geophones set in boreholes. It was revealed that the velocities of P and S waves continuously increased with depth. At Minami-Yamato Nunataks, velocities of both waves were obtained down to a depth of 100m in a bare ice region on 29 December 1983. The obtained velocities were constant from the surface to a depth of 100m, being 3.83km・s^<-1> for P wave and 2.01km・s^<-1> for S wave. P and S wave velocities at a depth of 100m at both sites were compared. It was found that the P wave velocity was almost the same at both sites, whereas the S wave velocity at Minami-Yamato Nunataks was larger than that at Mizuho Station, in spite of nearly identical ice density at both sites. The difference in the S wave velocity is discussed on the basis of difference in the crystal orientation. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
geographic East Antarctica
Mizuho
Yamato
Mizuho Station
geographic_facet East Antarctica
Mizuho
Yamato
Mizuho Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00001842
institution Open Polar
language English
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(35.583,35.583,-71.417,-71.417)
ENVELOPE(44.317,44.317,-70.683,-70.683)
op_collection_id ftnipr
op_relation Memoirs of National Institute of Polar Research. Special issue
39
165
172
AA00733561
https://nipr.repo.nii.ac.jp/record/1842/files/KJ00000012474.pdf
https://nipr.repo.nii.ac.jp/records/1842
publishDate 1985
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001842 2025-04-13T14:08:24+00:00 The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica Ishizawa, Kenji Mae, Shinji 1985-12 application/pdf https://nipr.repo.nii.ac.jp/record/1842/files/KJ00000012474.pdf https://nipr.repo.nii.ac.jp/records/1842 eng eng Memoirs of National Institute of Polar Research. Special issue 39 165 172 AA00733561 https://nipr.repo.nii.ac.jp/record/1842/files/KJ00000012474.pdf https://nipr.repo.nii.ac.jp/records/1842 1985 ftnipr 2025-03-19T10:19:56Z P(論文) At Mizuho Station (70°42'S, 44°20'E) velocity profiles of P and S waves down to a depth of 208m were measured on 30 July and 1 August 1983,the waves were generated by hitting an iron block set on the snow surface and traveled waves were detected by geophones set in boreholes. It was revealed that the velocities of P and S waves continuously increased with depth. At Minami-Yamato Nunataks, velocities of both waves were obtained down to a depth of 100m in a bare ice region on 29 December 1983. The obtained velocities were constant from the surface to a depth of 100m, being 3.83km・s^<-1> for P wave and 2.01km・s^<-1> for S wave. P and S wave velocities at a depth of 100m at both sites were compared. It was found that the P wave velocity was almost the same at both sites, whereas the S wave velocity at Minami-Yamato Nunataks was larger than that at Mizuho Station, in spite of nearly identical ice density at both sites. The difference in the S wave velocity is discussed on the basis of difference in the crystal orientation. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683)
spellingShingle Ishizawa, Kenji
Mae, Shinji
The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title_full The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title_fullStr The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title_full_unstemmed The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title_short The measurement of velocities of P and S waves in boreholes at Mizuho Station and Minami-Yamato Nunataks, East Antarctica
title_sort measurement of velocities of p and s waves in boreholes at mizuho station and minami-yamato nunataks, east antarctica
url https://nipr.repo.nii.ac.jp/record/1842/files/KJ00000012474.pdf
https://nipr.repo.nii.ac.jp/records/1842