Q of the Earth: Global, Regional, and Laboratory Studies:
Variations in seismic Q are sensitive to a much greater extent than are seismic velocity variations on factors such as temperature, fluid content, and the movement of solid state defects in the earth. For that reason an understanding of Q and its variation with position in the earth and with time sh...
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Weitere Verfasser: | , |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Basel
Birkhäuser Basel
1999
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Schriftenreihe: | Pageoph Topical Volumes
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Schlagworte: | |
Online-Zugang: | BTU01 Volltext |
Zusammenfassung: | Variations in seismic Q are sensitive to a much greater extent than are seismic velocity variations on factors such as temperature, fluid content, and the movement of solid state defects in the earth. For that reason an understanding of Q and its variation with position in the earth and with time should provide information in earth's tectonic evolution, as well as on aspects of its internal structure. Progress in understanding Q has suffered from difficulty in obtaining reliable amplitude data at global and temporary stations. Moreover, laboratory determinations of Q, until recently, were most often made at frequencies much higher than those measured by seismologists for waves propagating through the earth. Recent advances in seismic station distribution and quality, as well as in methodology at both high and low fequencies, have greatly improved the quality of observational data available to seismologists from global stations. Concurrent advances have been made in measuring Q using laboratory samples at frequencies that pertain to the earth and in theoretical understanding of seismic wave attenuation. Papers of this volume present new information on Q in the earth from several perspectives: methodology, results from global and regional observations of both body and surface waves, laboratory measurements, and theoretical understanding. The editors believe that we have reached a new threshold in Q studies and that advances in data quality and methodology will spur increased interest in this difficult, but interesting field |
Beschreibung: | 1 Online-Ressource (VI, 498 p. 60 illus., 7 illus. in color) |
ISBN: | 9783034887113 |
DOI: | 10.1007/978-3-0348-8711-3 |
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520 | |a Variations in seismic Q are sensitive to a much greater extent than are seismic velocity variations on factors such as temperature, fluid content, and the movement of solid state defects in the earth. For that reason an understanding of Q and its variation with position in the earth and with time should provide information in earth's tectonic evolution, as well as on aspects of its internal structure. Progress in understanding Q has suffered from difficulty in obtaining reliable amplitude data at global and temporary stations. Moreover, laboratory determinations of Q, until recently, were most often made at frequencies much higher than those measured by seismologists for waves propagating through the earth. Recent advances in seismic station distribution and quality, as well as in methodology at both high and low fequencies, have greatly improved the quality of observational data available to seismologists from global stations. Concurrent advances have been made in measuring Q using laboratory samples at frequencies that pertain to the earth and in theoretical understanding of seismic wave attenuation. Papers of this volume present new information on Q in the earth from several perspectives: methodology, results from global and regional observations of both body and surface waves, laboratory measurements, and theoretical understanding. The editors believe that we have reached a new threshold in Q studies and that advances in data quality and methodology will spur increased interest in this difficult, but interesting field | ||
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Datensatz im Suchindex
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spelling | Q of the Earth: Global, Regional, and Laboratory Studies edited by Brian J. Mitchell, Barbara Romanowicz Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 153 (1998), No. 2/3 Basel Birkhäuser Basel 1999 1 Online-Ressource (VI, 498 p. 60 illus., 7 illus. in color) txt rdacontent c rdamedia cr rdacarrier Pageoph Topical Volumes Variations in seismic Q are sensitive to a much greater extent than are seismic velocity variations on factors such as temperature, fluid content, and the movement of solid state defects in the earth. For that reason an understanding of Q and its variation with position in the earth and with time should provide information in earth's tectonic evolution, as well as on aspects of its internal structure. Progress in understanding Q has suffered from difficulty in obtaining reliable amplitude data at global and temporary stations. Moreover, laboratory determinations of Q, until recently, were most often made at frequencies much higher than those measured by seismologists for waves propagating through the earth. Recent advances in seismic station distribution and quality, as well as in methodology at both high and low fequencies, have greatly improved the quality of observational data available to seismologists from global stations. Concurrent advances have been made in measuring Q using laboratory samples at frequencies that pertain to the earth and in theoretical understanding of seismic wave attenuation. Papers of this volume present new information on Q in the earth from several perspectives: methodology, results from global and regional observations of both body and surface waves, laboratory measurements, and theoretical understanding. The editors believe that we have reached a new threshold in Q studies and that advances in data quality and methodology will spur increased interest in this difficult, but interesting field Earth Sciences Geology Earth sciences Dämpfung (DE-588)4010875-2 gnd rswk-swf Seismische Welle (DE-588)4180762-5 gnd rswk-swf (DE-588)4143413-4 Aufsatzsammlung gnd-content Seismische Welle (DE-588)4180762-5 s Dämpfung (DE-588)4010875-2 s DE-604 Mitchell, Brian J. edt Romanowicz, Barbara edt Erscheint auch als Druck-Ausgabe 9783764360498 https://doi.org/10.1007/978-3-0348-8711-3 Verlag URL des Erstveröffentlichers Volltext |
spellingShingle | Q of the Earth: Global, Regional, and Laboratory Studies Earth Sciences Geology Earth sciences Dämpfung (DE-588)4010875-2 gnd Seismische Welle (DE-588)4180762-5 gnd |
subject_GND | (DE-588)4010875-2 (DE-588)4180762-5 (DE-588)4143413-4 |
title | Q of the Earth: Global, Regional, and Laboratory Studies |
title_alt | Reprint from Pure and Applied Geophysics (PAGEOPH), Volume 153 (1998), No. 2/3 |
title_auth | Q of the Earth: Global, Regional, and Laboratory Studies |
title_exact_search | Q of the Earth: Global, Regional, and Laboratory Studies |
title_full | Q of the Earth: Global, Regional, and Laboratory Studies edited by Brian J. Mitchell, Barbara Romanowicz |
title_fullStr | Q of the Earth: Global, Regional, and Laboratory Studies edited by Brian J. Mitchell, Barbara Romanowicz |
title_full_unstemmed | Q of the Earth: Global, Regional, and Laboratory Studies edited by Brian J. Mitchell, Barbara Romanowicz |
title_short | Q of the Earth: Global, Regional, and Laboratory Studies |
title_sort | q of the earth global regional and laboratory studies |
topic | Earth Sciences Geology Earth sciences Dämpfung (DE-588)4010875-2 gnd Seismische Welle (DE-588)4180762-5 gnd |
topic_facet | Earth Sciences Geology Earth sciences Dämpfung Seismische Welle Aufsatzsammlung |
url | https://doi.org/10.1007/978-3-0348-8711-3 |
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