Titlebook: Digital Seismology and Fine Modeling of the Lithosphere; R. Cassinis,G. Nolet,G. F. Panza Book 1989 Springer Science+Business Media New Yo

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Digital Seismology and Fine Modeling of the Lithosphere

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Digital Seismology and Fine Modeling of the Lithosphere978-1-4899-6759-6

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Aspects of Acquisition and Interpretation of Deep Seismic Sounding Data,at present much more time has to be spent to digitize the analogue field data, which are still collected in Europe mostly with the same type of frequency-multiplex recording system MARS 66 or minor technical modifications thereof (Berckhemer, 1970), than for the preparation and realization of the fi

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Reference Model for Tomographic Imaging of the Upper Mantle Shear Velocity Structure Beneath Europeblems are to be expected. Fewer S data are available from the ISC and S delays are subject to larger errors due to identification problems and inaccuracies in the readings of the exact onsets. The choice of the starting or reference model to be used for tomographic inversions should be considered ca

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Broad-Band P-Wave Signals and Spectra from Digital Stations,e earthquake. For this reason, the spectral method in which the observed spectra are corrected for instrument response is probably a more reliable method for estimating seismic moments. Of course, if the instrument response of the seismograph does not include the corner frequency in its bandpass the

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Spencer G. Lucas,Lawrence H. Tannerat present much more time has to be spent to digitize the analogue field data, which are still collected in Europe mostly with the same type of frequency-multiplex recording system MARS 66 or minor technical modifications thereof (Berckhemer, 1970), than for the preparation and realization of the fi