Publication Year: 2015
DOI: https://doi.org/10.1002/2015gl064466
Abstract: Abstract We data accurate volume flux inversion. Conventional inversions without consideration of topographic to propagation effects may lead to large errors in the source estimate parameter estimate. The presented inversion technique will substantially improve the volume accuracy of eruption source parameter estimation (cf. mass eruption rate) fluxes during volcanic eruptions Show more
Authors:
Publication Year: 2003
DOI: https://doi.org/10.1029/2001jb001617
Abstract: We reexamine rigidity particularly for the smaller events in the data set. The times measurements determined from spectral ratios indicate no departure from constant the stress drop scaling down to the smallest events in our ratio data set ( M w 0.8). Our results indicate that between propagation effects can Show more
Authors:
Publication Year: 2001
DOI: https://doi.org/10.1785/0120000079
Abstract: To investigate the spectra (path averaged Q p = 100–400, Q s = Long 200–800). Source parameters are corrected for attenuation and radiation pattern. Both Valley static stress drops and apparent stresses range from approximately 0.01 caldera, to 30 MPa. Although static stress drops do not vary California, with seismic moment Show more
Authors:
Publication Year: 2003
DOI: https://doi.org/10.1016/s0377-0273(02)00499-7
Abstract: Not available
Authors:
Publication Year: 2002
DOI: https://doi.org/10.1016/s0012-821x(02)00857-9
Abstract: Not available
Authors:
Publication Year: 1993
DOI: https://doi.org/10.1111/j.1365-246x.1993.tb01488.x
Abstract: We present for appears to be substantially more efficient. 3-D Earth structure with respect to an arbitrary 3-D two starting model; one is a matrix formulation, and the second equivalent is a wavefield formulation. Both algorithms require the computation of algorithms accurate synthetic seismograms, but neither requires that any particular Show more
Authors:
Publication Year: 2011
DOI: https://doi.org/10.1111/j.1365-246x.2011.04938.x
Abstract: We observed with The principal value ratios of moment-tensor solutions can be approximated durations as 5:3:2, which is indicative of a combination of a of tensile crack and a cylinder, with the strike and dip 5–30 angle of the crack both being nearly 70°, and symmetry s axis of the Show more
Authors:
Publication Year: 2012
DOI: https://doi.org/10.1016/j.tecto.2012.12.015
Abstract: Not available
Authors:
Publication Year: 1990
DOI: https://doi.org/10.1111/j.1365-246x.1990.tb04574.x
Abstract: The first (e.g. and eigenfunctions. the present paper does not consider models with Woodhouse degenerate eigenstates, such as laterally homogeneous models. & Girnius, 1982; Tanimoto 1984) to compute the term partial derivatives of seismic waveforms. On the other hand, Tsuboi of & Geller (1987) first use the variational method to Show more
Authors:
Publication Year: 2008
DOI: https://doi.org/10.1016/j.jvolgeores.2008.03.033
Abstract: Not available
Authors:
Publication Year: 2013
DOI: https://doi.org/10.5047/eps.2013.03.002
Abstract: We deployed east was used to estimate the source locations of the explosion of earthquakes and weak continuous tremor. The sources of the explosion Shinmoedake earthquakes were beneath the crater at depths of −0.5–1 km volcano, above sea level, while the source of the weak continuous in tremor was beneath Show more
Authors:
Publication Year: 2013
DOI: https://doi.org/10.1007/s00445-013-0710-9
Abstract: Not available
Authors:
Publication Year: 2013
DOI: https://doi.org/10.1007/s00445-013-0709-2
Abstract: Not available
Authors:
Publication Year: 2002
DOI: https://doi.org/10.1016/s0377-0273(01)00298-0
Abstract: Not available
Authors:
Publication Year: 2003
DOI: https://doi.org/10.1046/j.1365-246x.2003.01936.x
Abstract: The finite dynamics, magmatic fluid in the reservoir before the eruption. Magma transfer seismic between the reservoir and conduit is triggered by the instantaneous radiation, removal of the plug, and the eruption occurs when the and pressure at the conduit orifice exceeds the material strength of crustal the lid capping Show more
Authors:
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