The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern?
On 1986 August 1 a small seismic disturbance occurred to the east of a Soviet nuclear test site at Novaya Zemlya. Reported attempts to identify the nature of the source using only short-period seismological data recorded at regional distances were unsuccessful. However, by using teleseismic P-wave d...
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1989
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fthighwire:oai:open-archive.highwire.org:gji:98/3/565 2023-05-15T17:47:13+02:00 The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? Marshall, P. D. Stewart, R. C. Lilwall, R. C. 1989-09-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/98/3/565 https://doi.org/10.1111/j.1365-246X.1989.tb02290.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/98/3/565 http://dx.doi.org/10.1111/j.1365-246X.1989.tb02290.x Copyright (C) 1989, Oxford University Press Articles TEXT 1989 fthighwire https://doi.org/10.1111/j.1365-246X.1989.tb02290.x 2016-11-16T17:36:10Z On 1986 August 1 a small seismic disturbance occurred to the east of a Soviet nuclear test site at Novaya Zemlya. Reported attempts to identify the nature of the source using only short-period seismological data recorded at regional distances were unsuccessful. However, by using teleseismic P-wave data it is possible to identify the source as an earthquake which occurred within the crust at a depth of 24 km. The source is shown to have a double-couple mechanism with a well-constrained fault-plane solution. The identification as an earthquake is supported by the m b : M s , evidence. Text Novaya Zemlya HighWire Press (Stanford University) Geophysical Journal International 98 3 565 573 |
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HighWire Press (Stanford University) |
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English |
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Articles |
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Articles Marshall, P. D. Stewart, R. C. Lilwall, R. C. The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
topic_facet |
Articles |
description |
On 1986 August 1 a small seismic disturbance occurred to the east of a Soviet nuclear test site at Novaya Zemlya. Reported attempts to identify the nature of the source using only short-period seismological data recorded at regional distances were unsuccessful. However, by using teleseismic P-wave data it is possible to identify the source as an earthquake which occurred within the crust at a depth of 24 km. The source is shown to have a double-couple mechanism with a well-constrained fault-plane solution. The identification as an earthquake is supported by the m b : M s , evidence. |
format |
Text |
author |
Marshall, P. D. Stewart, R. C. Lilwall, R. C. |
author_facet |
Marshall, P. D. Stewart, R. C. Lilwall, R. C. |
author_sort |
Marshall, P. D. |
title |
The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
title_short |
The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
title_full |
The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
title_fullStr |
The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
title_full_unstemmed |
The seismic disturbance on 1986 August 1 near Novaya Zemlya: a source of concern? |
title_sort |
seismic disturbance on 1986 august 1 near novaya zemlya: a source of concern? |
publisher |
Oxford University Press |
publishDate |
1989 |
url |
http://gji.oxfordjournals.org/cgi/content/short/98/3/565 https://doi.org/10.1111/j.1365-246X.1989.tb02290.x |
genre |
Novaya Zemlya |
genre_facet |
Novaya Zemlya |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/98/3/565 http://dx.doi.org/10.1111/j.1365-246X.1989.tb02290.x |
op_rights |
Copyright (C) 1989, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1989.tb02290.x |
container_title |
Geophysical Journal International |
container_volume |
98 |
container_issue |
3 |
container_start_page |
565 |
op_container_end_page |
573 |
_version_ |
1766151577350963200 |