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

Language: English

Published by Birkhäuser, 2001

3764365501 / 9783764365509

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Seller: AHA-BUCH GmbH, Einbeck, GermanyAHA-BUCH GmbH

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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).

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Title
Monitoring the Comprehensive Nuclear-Test-Ban Treaty : Regional Wave Propagation and Crustal Structure
Author
Brian J. Mitchell
Publisher
Birkhäuser
Publication year
2001
Condition
Neu
Binding
Taschenbuch
Language
English
ISBN 10
3764365501
ISBN 13
9783764365509
Item weight
409 grams
Dimensions
244x170x13 mm

AHA-BUCH GmbH

Einbeck, Germany

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