Gerveny 1985b which describes correctly the path and the. Atmospheric infrasound propagation modelling using the. Computation of synthetic seismograms with the reflectivity. Chapter 1 literature the following list contains only books, that treat the propagation of elastic waves and a few text books on continuum mechanics. The software development follows closely the tutorial published by muller 1985. Ma et al 2004, which follows the algorithm described by muller 1985. Seismic modelling with the reflectivity method crewes. The desired speed of the vehicle is set into a digital memory bank and the instantaneous actual speed of the vehicle is determined by a digital readout. Reflectivity method for geomechanical equilibria geophysical. Reflectivity modelling is always carried out in a cylindrical coordinate system. Dogrusal interpolasyon metodu false position method or regula falsi method duration. Reflectivity modeling of a groundpenetratingradar profile of a saturated fluvial formation article pdf available in geophysics 7 may 2006 with 78 reads how we measure reads.
The elastic diffusiveviscous wave equation is firstly investigated by considering the shear motion. Wave propagation in complicated earth models can be simulated, thanks to so. Prestack ava joint inversion of pp and ps waves using the. Pdf mueller matrix measurements and modeling pertaining. Journal of geophysics zeitschrift fur geophysik 58. Then, we use the extended reflectivity method to simulate the propagation of diffusiveviscous wave without considering the shear waves. The earth model consists of a stack of flat, elastic layers figure 1.
This allows to introduce a generalization of the kennett reflectivity method, which is applicable to arbitrary. The reflectivity method is applied to the interpretation of observations along a profile in central europe. The reflectivity method for different source and receiver structures and comparison with grf data kind, r. Reflectivity modeling for stratified anelastic media crewes. Generalisations of the laplacerungelenz vector 341 3 conservation of the direction of angular momentum only 360 3. Complete synthetic seismograms for a spherically symmetric. The reflectivity method is a technique that has been applied to generating synthetic seismograms for point sources in a layered medium. The field of application of these methods is the comparison with observed seismograms obtained from refraction studies of the earths crust and upper mantle. Mullers method takes a similar approach, but projects a parabola through three points fig. Reflectivity method for modeling the propagation of. Pdf reflectivity modeling of a groundpenetratingradar. We present a new method to calculate complete synthetic seismograms for a spherically symmetric earth model which uses neither eigenfrequencies and eigenfunctions nor an earthflattening transformation. The reflectivity method was originally developed by fuches and muller 1971. Each layer is n described by its elastic properties.
Finally, we simulate the propagation of elastic diffusiveviscous waves in diplayered media. The method consists of deriving the coefficients of the parabola that goes. The reflectivity method models refraction, reflection, multiples, attenuation and dispersion. Focal parameters of some friuli earthquakes 19761979 using complete theoretical seismograms barbano, m.
The full mueller matrix for a spectralon white reflectance standard was measured in the incidence plane, to obtain the polarization state of the scattered light for different angles of illumination. A note on the equivalence of three major propagator algorithms for. Most current prestack ava joint inversion methods are based on the exact. Margrave abstract numerical seismic modelling is a powerful tool in seismic imaging, interpretation and inversion. The reflectivity method theory is discussed in details by kennett 1983.
1119 839 156 1139 96 1106 1011 514 292 731 224 1428 476 576 561 1173 1394 925 662 595 1163 1470 1366 674 1408 599 332 987 899 1403 1434 1359 1139 559 197 287 1280 74 515 636 463 839 1472 1106 1041 597 240 670