Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya
SUMMARY. - The analysis of the travel times of the P waves generated by six underground nuclear explosions in Novaya Zemlya shows notable early arrivals (oo4sec) at the Fennoscandia stations. These observations, together with a marked linear dependence of the travel times on the epicentral distance...
Published in: | Annals of Geophysics |
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1977
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Online Access: | https://doi.org/10.4401/ag-4815 https://doaj.org/article/9381a24cf84a4a5a808e0c9a1c79c199 |
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ftdoajarticles:oai:doaj.org/article:9381a24cf84a4a5a808e0c9a1c79c199 2023-05-15T16:11:56+02:00 Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya B. FEDERICO A. BOTTARI 1977-06-01T00:00:00Z https://doi.org/10.4401/ag-4815 https://doaj.org/article/9381a24cf84a4a5a808e0c9a1c79c199 EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/4815 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-4815 1593-5213 2037-416X https://doaj.org/article/9381a24cf84a4a5a808e0c9a1c79c199 Annals of Geophysics, Vol 30, Iss 1-2, Pp 83-106 (1977) Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 1977 ftdoajarticles https://doi.org/10.4401/ag-4815 2022-12-31T04:11:00Z SUMMARY. - The analysis of the travel times of the P waves generated by six underground nuclear explosions in Novaya Zemlya shows notable early arrivals (oo4sec) at the Fennoscandia stations. These observations, together with a marked linear dependence of the travel times on the epicentral distance throughout the interval 8.5 < / J ° < 20.4. were evaluated with the aim of producing a satisfactory model for the upper mantle of the Baltic zone. In particular, there appears a considerable mantle zone with almost uniform velocity, or at least, with not of increasing velocity. This mantle zone is delimited above by a discontinuity at the 86 km depth (v = 8.45 km/sec), and delimited below by the «20° discontinuity» (h = 507 km; v = 10.56 km/sec). The proposed model is amply verified on the basis of the foreseen travel times compared with the corresponding ones, observed from a fair number of impulses associated with teleseismic Pn, noticeable as far as 40°, and from phases reflected and refracted on the discontinuity at 507 km. Article in Journal/Newspaper Fennoscandia Novaya Zemlya Directory of Open Access Journals: DOAJ Articles Annals of Geophysics 30 1-2 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 B. FEDERICO A. BOTTARI Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
topic_facet |
Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
description |
SUMMARY. - The analysis of the travel times of the P waves generated by six underground nuclear explosions in Novaya Zemlya shows notable early arrivals (oo4sec) at the Fennoscandia stations. These observations, together with a marked linear dependence of the travel times on the epicentral distance throughout the interval 8.5 < / J ° < 20.4. were evaluated with the aim of producing a satisfactory model for the upper mantle of the Baltic zone. In particular, there appears a considerable mantle zone with almost uniform velocity, or at least, with not of increasing velocity. This mantle zone is delimited above by a discontinuity at the 86 km depth (v = 8.45 km/sec), and delimited below by the «20° discontinuity» (h = 507 km; v = 10.56 km/sec). The proposed model is amply verified on the basis of the foreseen travel times compared with the corresponding ones, observed from a fair number of impulses associated with teleseismic Pn, noticeable as far as 40°, and from phases reflected and refracted on the discontinuity at 507 km. |
format |
Article in Journal/Newspaper |
author |
B. FEDERICO A. BOTTARI |
author_facet |
B. FEDERICO A. BOTTARI |
author_sort |
B. FEDERICO |
title |
Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
title_short |
Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
title_full |
Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
title_fullStr |
Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
title_full_unstemmed |
Travel time analysis of P waves arising from six underground nuclear explosion at Novaya Zemlya |
title_sort |
travel time analysis of p waves arising from six underground nuclear explosion at novaya zemlya |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
publishDate |
1977 |
url |
https://doi.org/10.4401/ag-4815 https://doaj.org/article/9381a24cf84a4a5a808e0c9a1c79c199 |
genre |
Fennoscandia Novaya Zemlya |
genre_facet |
Fennoscandia Novaya Zemlya |
op_source |
Annals of Geophysics, Vol 30, Iss 1-2, Pp 83-106 (1977) |
op_relation |
http://www.annalsofgeophysics.eu/index.php/annals/article/view/4815 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-4815 1593-5213 2037-416X https://doaj.org/article/9381a24cf84a4a5a808e0c9a1c79c199 |
op_doi |
https://doi.org/10.4401/ag-4815 |
container_title |
Annals of Geophysics |
container_volume |
30 |
container_issue |
1-2 |
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1765997144394694656 |