Evidence of a laterally variable lower mantle structure from P- and S-waves
Examples of Gräfenberg-array data showing anomalous P -waves which typically arrive 3–5 s after the direct P -wave and which have a slowness 0.7–0.8 s deg-1 smaller than direct P are presented. This additional phase is most frequently observed for events located in the NE portion of the southern Kur...
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1990
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fthighwire:oai:open-archive.highwire.org:gji:102/1/231 2023-05-15T16:30:25+02:00 Evidence of a laterally variable lower mantle structure from P- and S-waves Weber, M. Davis, J. P. 1990-07-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/102/1/231 https://doi.org/10.1111/j.1365-246X.1990.tb00544.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/102/1/231 http://dx.doi.org/10.1111/j.1365-246X.1990.tb00544.x Copyright (C) 1990, Oxford University Press Articles TEXT 1990 fthighwire https://doi.org/10.1111/j.1365-246X.1990.tb00544.x 2015-02-28T17:48:17Z Examples of Gräfenberg-array data showing anomalous P -waves which typically arrive 3–5 s after the direct P -wave and which have a slowness 0.7–0.8 s deg-1 smaller than direct P are presented. This additional phase is most frequently observed for events located in the NE portion of the southern Kurile Island subduction zone 73°-80° from Gräfenberg, but systematically disappears for events in the SW portion of this zone. Because of the magnitude of the slowness difference, these observations cannot be attributed to a complex source rupture process nor to multipathing through the descending slab. Likewise, they may not be accounted for by near-receiver structure because these phases are not seen for all Kurile events. If present they appear at all stations of the array but they follow direct P too closely to be a multiple from the Mono. Therefore, we conclude they are very likely caused by lower mantle velocity structure. The most likely explanation is the presence of a P velocity jump of about 3 per cent approximately 290 km above the core-mantle boundary, since such a reflector in the lowermost mantle not only gives a good fit of traveltimes and slowness but is also able to model the waveform and the amplitudes of this additional P phase. The distribution of bounce points on this reflector for the Kurile events indicates a lateral extension of this velocity anomaly under northern Siberia of about 150 km by at least 200 km. The best fitting S -wave model has a reflector in the same depth, but the velocity contrast seems to be only about 2 per cent suggesting a different behaviour of the P and S velocity in D″. Few events from other regions in this distance range are suitable for a definitive analysis of this kind. From among this group some observations indicate a lower mantle anomaly under the Lomonosow Ridge and under northern Greenland; but since the lower mantle under western Siberia, northern Novaya Zemlya, the Azores Islands region and the USSR-Afghanistan border region does not produce an additional phase ... Text Greenland Novaya Zemlya Siberia HighWire Press (Stanford University) Greenland Geophysical Journal International 102 1 231 255 |
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English |
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Articles |
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Articles Weber, M. Davis, J. P. Evidence of a laterally variable lower mantle structure from P- and S-waves |
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Articles |
description |
Examples of Gräfenberg-array data showing anomalous P -waves which typically arrive 3–5 s after the direct P -wave and which have a slowness 0.7–0.8 s deg-1 smaller than direct P are presented. This additional phase is most frequently observed for events located in the NE portion of the southern Kurile Island subduction zone 73°-80° from Gräfenberg, but systematically disappears for events in the SW portion of this zone. Because of the magnitude of the slowness difference, these observations cannot be attributed to a complex source rupture process nor to multipathing through the descending slab. Likewise, they may not be accounted for by near-receiver structure because these phases are not seen for all Kurile events. If present they appear at all stations of the array but they follow direct P too closely to be a multiple from the Mono. Therefore, we conclude they are very likely caused by lower mantle velocity structure. The most likely explanation is the presence of a P velocity jump of about 3 per cent approximately 290 km above the core-mantle boundary, since such a reflector in the lowermost mantle not only gives a good fit of traveltimes and slowness but is also able to model the waveform and the amplitudes of this additional P phase. The distribution of bounce points on this reflector for the Kurile events indicates a lateral extension of this velocity anomaly under northern Siberia of about 150 km by at least 200 km. The best fitting S -wave model has a reflector in the same depth, but the velocity contrast seems to be only about 2 per cent suggesting a different behaviour of the P and S velocity in D″. Few events from other regions in this distance range are suitable for a definitive analysis of this kind. From among this group some observations indicate a lower mantle anomaly under the Lomonosow Ridge and under northern Greenland; but since the lower mantle under western Siberia, northern Novaya Zemlya, the Azores Islands region and the USSR-Afghanistan border region does not produce an additional phase ... |
format |
Text |
author |
Weber, M. Davis, J. P. |
author_facet |
Weber, M. Davis, J. P. |
author_sort |
Weber, M. |
title |
Evidence of a laterally variable lower mantle structure from P- and S-waves |
title_short |
Evidence of a laterally variable lower mantle structure from P- and S-waves |
title_full |
Evidence of a laterally variable lower mantle structure from P- and S-waves |
title_fullStr |
Evidence of a laterally variable lower mantle structure from P- and S-waves |
title_full_unstemmed |
Evidence of a laterally variable lower mantle structure from P- and S-waves |
title_sort |
evidence of a laterally variable lower mantle structure from p- and s-waves |
publisher |
Oxford University Press |
publishDate |
1990 |
url |
http://gji.oxfordjournals.org/cgi/content/short/102/1/231 https://doi.org/10.1111/j.1365-246X.1990.tb00544.x |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Novaya Zemlya Siberia |
genre_facet |
Greenland Novaya Zemlya Siberia |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/102/1/231 http://dx.doi.org/10.1111/j.1365-246X.1990.tb00544.x |
op_rights |
Copyright (C) 1990, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1990.tb00544.x |
container_title |
Geophysical Journal International |
container_volume |
102 |
container_issue |
1 |
container_start_page |
231 |
op_container_end_page |
255 |
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1766020145562517504 |