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...
Main Authors: | , |
---|---|
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 |
_version_ | 1829312435479117824 |
---|---|
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 |