Spectral discrimination analysis of Eurasian nuclear tests and earthquakesrecorded by the Israel Seismic Network and the NORESS array

Citation
Y. Gitterman et al., Spectral discrimination analysis of Eurasian nuclear tests and earthquakesrecorded by the Israel Seismic Network and the NORESS array, PHYS E PLAN, 113(1-4), 1999, pp. 111-129
Citations number
21
Categorie Soggetti
Earth Sciences
Journal title
PHYSICS OF THE EARTH AND PLANETARY INTERIORS
ISSN journal
00319201 → ACNP
Volume
113
Issue
1-4
Year of publication
1999
Pages
111 - 129
Database
ISI
SICI code
0031-9201(199906)113:1-4<111:SDAOEN>2.0.ZU;2-Z
Abstract
The energy spectral ratio and the innovative spectral semblance discriminan ts, successfully performed previously on a local Israeli events, were verif ied on teleseismic short-period recordings. The events tested include 29 nu clear explosions and 41 earthquakes (m(b) = 5.2-6.5), mainly from China and Kazakhstan, recorded by the Israel Seismic Network (ISN) and the NORESS ar ray. A 15-s window comprising P- and P-coda waves was selected for the anal ysis. The 'semblance' statistic commonly used in seismic prospecting for ph ase correlation in the time domain was modified and utilized as a measure o f coherency of the smoothed spectra across the network/array. The semblance and the average spectral ratio of low-to-high frequency energy were evalua ted, using a subset of 7-10 stations for a given event. Semblance and spect ral ratio values, calculated from ISN seismograms, were found to be higher for earthquakes, where the analyzed waves are richer in low-frequency energ y and have more coherent spectral shapes than explosions. These observation s are contrary to those observed for local events. The best performance is provided in the frequency bands (0.6-1 Hz)/(1-3 Hz) (for the ratio) and (0. 6-2 Hz) (for the semblance). Joint application of the two discriminants sho wed almost full separation (95%) between the two populations. Some explosio ns exhibited pronounced minima (nulls) near 1 Hz which could be interpreted in terms of interference of P- and pP-waves from a source at the depth of several hundreds of meters. Nevertheless, this feature could not be utilize d as a discriminant: many explosions revealed strong variability of this mi nimum across the ISN network and some earthquakes also distinctly exhibited this feature. The ISN and NORESS discrimination performances were compared . The latter records showed the same (as the ISN) relation between spectral ratio values for earthquakes and explosions, whereas the character of semb lance was reversed. The ratios in the frequency bands (0.6-0.8 Hz)/(0.6-10 Hz) yield full separation of the two populations. In general, the spectral ratio performance appears to be better for NORESS recordings! whereas the s pectral semblance is better for the ISN data. (C) 1999 Elsevier Science B.V . All rights reserved.