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Regional phase excitation and propagation in the Lop Nor region of central Asia and implications for P/Lg discriminants

Journal Article · · Journal of Geophysical Research
 [1];  [2]
  1. Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York (United States)
  2. Los Alamos National Laboratory, Los Alamos, New Mexico (United States)

{ital Pn} and {ital Lg} spectra for Lop Nor explosions and nearby earthquakes were analyzed for source and propagation effects using a modified inversion method of {ital Xie} [1993]. Spectral analyses were performed on waveform data from Incorporated Research Institution for Seismology, Chinese Digital Seismic Network, Kazakhstan, and Krgyzstan networks. {ital Pn} amplitude variations of a factor of 20 are observed across the small-aperture ({lt} 200 km) Kyrgyzstan network, and are probably related to three-dimensional Moho structure close to the network. Comparisons of {ital Pn} amplitudes and spectral ratios provide evidence for nonisotropic radiation pattern effects in the case of earthquakes and overshoot in explosion time histories. Complex source effects are born out in our inversion results: (1) logarithm of seismic moment (M{sub 0}) from {ital Pn} and {ital Lg} spectra scale linearly with body wave magnitude (m{sub b}) for explosions (5.0{le}m{sub b}{le}6.0) and for earthquakes (4.0{le}m{sub b}{le}5.5); (2) Pn; M{sub 0} estimates are similar to Lg; M{sub 0} for earthquakes but are higher than Lg; M{sub 0} for explosions; (3) corner frequency f{sub c} scale as quarter root of M{sub 0} for explosions and cube root for earthquakes; (4) at the same M{sub 0} level, Pn; f{sub c} are 4{endash}5 times higher than Lg; f{sub c} for earthquakes and explosions; and (5) {ital Pn} source spectra are characterized by significant overshoot for explosions. Our results suggest that the cause of maximum separation between earthquake and explosion populations on plots of P/Lg spectral ratios, which typically occurs for frequencies above explosion Pn f{sub c} (between 2 and 4 Hz for explosions in this study), may be related to overshoot in the reduced velocity potential. {copyright} 1999 American Geophysical Union

Research Organization:
Los Alamos National Laboratory
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
700955
Journal Information:
Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: B1 Vol. 104; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English