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Monitoring the Comprehensive Nuclear-Test-Ban Treaty: Source Processes and Explosion Yield Estimation

✍ Scribed by Göran Ekström, Marvin Denny, John R. Murphy (auth.), Göran Ekström, Marvin Denny, John R. Murphy (eds.)


Publisher
Birkhäuser Basel
Year
2001
Tongue
English
Leaves
425
Series
Pageoph Topical Volumes
Edition
1
Category
Library

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✦ Synopsis


Pure appl. geophys., by 161 nations. Entry of the treaty into force, however, is still uncertain since it requires ratification by all 44 nations that have some nuclear capability and, as of 15 June 2001, only 31 of those nations have done so. Although entry of the CTBT into force is still uncertain, seismologists and scientists in related fields, such as radionuclides, have proceeded with new research on issues relevant to monitoring compliance with it. Results of much of that research may be used by the International Monitoring System, headquartered in Vienna, and by several national centers and individual institutions, to monitor compliance with the CTBT. New issues associated with CTBT monitoring in the 21st century have presented scientists with many new challenges. They must be able to effectively monitor com­ pliance by several countries that have not previously been nuclear powers. Effective monitoring requires that we be able to detect and locate much smaller nuclear events than ever before and to distinguish them from small earthquakes and other types of explosions. We must have those capabilities in regions that are seismically active and geologically complex, and where seismic waves might not propagate efficiently.

✦ Table of Contents


Front Matter....Pages i-vi
Introduction....Pages 1863-1865
Front Matter....Pages 1867-1867
Effects of Rock Damage on Seismic Waves Generated by Explosions....Pages 1869-1908
Wave Generation from Explosions in Rock Cavities....Pages 1909-1949
Regional Magnitude Scaling, Transportability, and M s :m b Discrimination at Small Magnitudes....Pages 1951-2015
Shallow Velocity Structure at the Shagan River Test Site in Kazakhstan....Pages 2017-2039
The Kirovskiy Explosion of September 29, 1996: Example of a CTB Event Notification for a Routine Mining Blast....Pages 2041-2058
Source Directivity, Signal Decorrelation, Spectral Modulation and Analysis of Spatio-temporal Patterns of Multiple Explosions....Pages 2059-2076
Seismic Source Characteristics of Soviet Peaceful Nuclear Explosions....Pages 2077-2101
Front Matter....Pages 2103-2103
Seismic Source Characteristics of Nuclear Explosions in Water-filled Cavities....Pages 2105-2121
Application of Network-averaged Teleseismic P-wave Spectra to Seismic Yield Estimation of Underground Nuclear Explosions....Pages 2123-2171
Effects of Source RDP Models and Near-source Propagation: Implication for Seismic Yield Estimation....Pages 2173-2216
Yield Estimation for Semipalatinsk Underground Nuclear Explosions Using Seismic Surface-wave Observations at Near-regional Distances....Pages 2217-2226
Yield Estimation from Surface-wave Amplitudes....Pages 2227-2251
Teleseismic Lg of Semipalatinsk and Novaya Zemlya Nuclear Explosions Recorded by the GRF (Gräfenberg) Array: Comparison with Regional Lg (BRV) and their Potential for Accurate Yield Estimation....Pages 2253-2274
Classical and Bayesian Seismic Yield Estimation: The 1998 Indian and Pakistani Tests....Pages 2275-2290

✦ Subjects


Geophysics/Geodesy


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