Journal ArticleDOI
Source solutions and station residuals from long‐period waveform inversion of deep events
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In this paper, an earth model based on PREM with different source and receiver structures and the introduction of time delays were determined together with the moment tensor components of the source by an iterative correlation method.Abstract:
Deep earthquakes of up to moderate size have been analyzed by a long-period waveform inversion of Global Digital Seismographic Network data where the use of a point source model proved to be adequate, but the use of a standard earth model was inadequate without modification. Modifications include calculations in an earth model based on PREM but with different source and receiver structures and the introduction of time delays which were determined together with the moment tensor components of the source by an iterative correlation method. The moment tensor components are in accordance With the pattern of stress release in other work, but results for the seismic moment differ somewhat and there is no compelling evidence for deviations from a double couple mechanism. The time delays were inverted to find the source centroid depths and time shifts and the station residuals. There is no baseline effect in the times of source duration which could be explained by a simple circular source model, but there is such an effect in the station residuals together with a distance trend especially for S. Part of the baselines may be an effect of bias in origin times, but the pattern of S residuals in particular suggests also possible modifications of the standard model.read more
Citations
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Journal ArticleDOI
Global upper mantle structure from long-period differential travel times
Robert L. Woodward,Guy Masters +1 more
TL;DR: In this article, the authors made over ten thousand measurements of PP-P and SS-S differential travel times from long-period Global Digital Seismograph Network recordings of all events with mb ≥ 5.5 which occurred during the years 1976 to 1986.
Journal ArticleDOI
Estimation of earthquake source parameters by the inversion of waveform data: Global seismicity, 1981-1983
TL;DR: In this article, a waveform inversion algorithm, based on optimal filter theory, has been applied to the P waves from 260 of the largest earthquakes occurring during the years 1981 through 1983, and estimates of average focal depth, scalar moment, and deviatoric source mechanism have been obtained.
Journal ArticleDOI
Earthquakes with non--double-couple mechanisms.
TL;DR: Current research focuses on whether fault complexity explains most observed non-double-couple earthquakes and to what extent ordinary earthquakes have non—double-Couple components.
Journal ArticleDOI
Waveform modelling using locked-mode synthetic and differential seismograms: application to determination of the structure of Mexico
Joan Gomberg,T. Guy Masters +1 more
TL;DR: In this paper, the authors developed algorithms for modeling seismic waveforms in order to constrain regional Earth structure, where the seismogram is represented as a sum of locked-mode travelling waves in a layered medium.
Journal ArticleDOI
Significance of non-double couple components of deep and intermediate-depth earthquakes: implications from moment tensor inversions of long-period seismic waves
Keiko Kuge,Hitoshi Kawakatsu +1 more
TL;DR: In this paper, the non-double couple components in source moment tensors of intermediate-depth and deep earthquakes are significant and appear to respond to the state of predominant strain release within slabs, which is partially or fully induced by the sources themselves or by slab structures near the sources.
References
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Journal ArticleDOI
Preliminary reference earth model
TL;DR: In this paper, a large data set consisting of about 1000 normal mode periods, 500 summary travel time observations, 100 normal mode Q values, mass and moment of inertia have been inverted to obtain the radial distribution of elastic properties, Q values and density in the Earth's interior.
Journal ArticleDOI
Theoretical basis of some empirical relations in seismology
Hiroo Kanamori,Don L. Anderson +1 more
TL;DR: In this article, an empirical relation involving seismic moment M, energy E, magnitude M, and fault dimension L (or area S) is discussed on the basis of an extensive set of earthquake data (M_S ≧ 6) and simple crack and dynamic dislocation models.
Journal ArticleDOI
Determination of earthquake source parameters from waveform data for studies of global and regional seismicity
TL;DR: In this article, an initial moment tensor is derived using one of the variations of the method described in detail by Gilbert and Dziewonski (1975), where perturbations to the elements of the moments are found simultaneously with changes in the hypocentral parameters.
Journal ArticleDOI
An Application of Normal Mode Theory to the Retrieval of Structural Parameters and Source Mechanisms from Seismic Spectra
TL;DR: In this paper, the elastic-gravitational free oscillations of the Earth are used to derive procedures for resolving nearly degenerate multiplets of normal modes of an earthquake point source.
Journal ArticleDOI
Distribution of stresses in the descending lithosphere from a global survey of focal‐mechanism solutions of mantle earthquakes
Bryan L. Isacks,Peter Molnar +1 more
TL;DR: A region-byregion analysis of 204 reliable focal-mechanism solutions for deep and intermediate-depth earthquakes strongly supports the idea that portions of the lithosphere that descend into the mantle are slablike stress guides that align the earthquake-generating stresses parallel to the inclined seismic zones as mentioned in this paper.
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