Monitoring the Comprehensive Nuclear-Test-Ban Treaty | Regional Wave Propagation and Crustal Structure

Brian J. Mitchell (u. a.)

ISBN 10: 3764365501 ISBN 13: 9783764365509

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Synopsis :

Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35� (e. g., MOLNAR and OLIVER, 1969; HUESTIS et aI., 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al., 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al., 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995).

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Titre : Monitoring the Comprehensive ...
�diteur : Springer Basel
Date d'�dition : 2001
Reliure : Taschenbuch
Etat : Neu

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Monitoring the Comprehensive Nuclear Test Ban Treaty Regional Wave Propagation and Crystal Structure.

Edit� par Birkhäuser., 2001

ISBN 10 : 3764365501 ISBN 13 : 9783764365509

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2001th ed. 18 x 25 cm. 228 pages. Paperback. Versand aus Deutschland / We dispatch from Germany via Air Mail. Einband besto�en, daher M�ngelexemplar gestempelt, sonst sehr guter Zustand. Imperfect copy due to slightly bumped cover, apart from this in very good condition. Stamped. Sprache: Englisch. N� de r�f. du vendeur 6377VB

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty

Patton, H. J.|Mitchell, Brian J.

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Kartoniert / Broschiert. Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) . N� de r�f. du vendeur 5279443

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty : Regional Wave Propagation and Crustal Structure

Brian J. Mitchell

Edit� par Birkh�user Basel, Springer Basel, 2001

ISBN 10 : 3764365501 ISBN 13 : 9783764365509

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Taschenbuch. Etat : Neu. Druck auf Anfrage Neuware - Printed after ordering - Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35� (e. g. , MOLNAR and OLIVER, 1969; HUESTIS et aI. , 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al. , 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al. , 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995). N� de r�f. du vendeur 9783764365509

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty

Brian J. Mitchell

Edit� par Birkh�user Basel, Springer Basel Sep 2001, 2001

ISBN 10 : 3764365501 ISBN 13 : 9783764365509

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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35� (e. g. , MOLNAR and OLIVER, 1969; HUESTIS et aI. , 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al. , 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al. , 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995). 232 pp. Englisch. N� de r�f. du vendeur 9783764365509

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty

H. J. Patton

Edit� par Springer, Basel, Birkh�user Basel, Birkh�user Sep 2001, 2001

ISBN 10 : 3764365501 ISBN 13 : 9783764365509

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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Regional seismograms are dominated by the phases Pn, Pg, Sn, and Lg. More often Sn and Lg are used to infer the attenuation structure of the lithosphere. The seismic phase Sn is a high-frequency shear-wave (typically from 1 to 4 Hz and occasionally higher) that travels in the lithospheric mantle above the negative velocity gradient which usually marks the lithosphere-asthenosphere boundary. Sn has been reported out to distances of 35� (e. g. , MOLNAR and OLIVER, 1969; HUESTIS et aI. , 1973). Sn arrives as a high-frequency wave train lasting tens of seconds and up to 1 to 2 minutes. Sn velocities are typically 4. 7 km/s in stable continental and oceanic lithosphere (HUESTIS et al. , 1973) and as low as 4. 3 km/s (KADINSKY-CADE et al. , 1981) in more tectonically active regions. Lg is a complex short period guided wave consisting of high-frequency P and S energy which travels primarily in the earth's crust at frequencies typically between 0. 5 and 5 Hz. It has been modeled as higher-mode Love and Rayleigh waves as well as a sequence of multiply reflected post-critical S waves trapped in a crustal guide (BOUCHON, 1982; KENNETT, 1986; BOSTOCK and KENNETT, 1990). Lg has been observed not to propagate in oceanic or very thin continental crust (PRESS and EWING, 1952; SEARLE, 1975; ZHANG and LAY, 1995). 211 pp. Englisch. N� de r�f. du vendeur 9783764365509

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Monitoring the Comprehensive Nuclear Test Ban Treaty Regional Wave Propagation and Crystal Structure

Edit� par Birkh�user, 2001

ISBN 10 : 3764365501 ISBN 13 : 9783764365509

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty : Regional Wave Propagation and Crustal Structure

Patton, Howard J. (EDT); Mitchell, Brian J. (EDT)

Edit� par Birkh�user, 2001

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Monitoring the Comprehensive Nuclear-Test-Ban Treaty

. Ed(s): Patton, H. J.; Mitchell, Brian J.

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Etat : New. Includes papers that investigate regional variations of elastic and anelastic properties of Eurasia, the blockage of regional phases by sedimentary basins, methods for modeling regional wave propagation and for calibrating seismic wave paths in order to extract amplitude variations and source parameters. Editor(s): Patton, H. J.; Mitchell, Brian J. Series: Pageoph Topical Volumes. Num Pages: 216 pages, 42 black & white illustrations, 11 colour illustrations, biography. BIC Classification: PHN; RBC. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly; (UU) Undergraduate. Dimension: 244 x 170 x 12. Weight in Grams: 496. . 2001. Paperback. . . . . N� de r�f. du vendeur V9783764365509

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