Extensions of the reflectivity method

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Abstract

The reflectivity method for the computation of theoretical seismograms is extended to include a dislocation point source of arbitrary orientation buried in a layered medium. The second extension is a change in the numerical integration over the circular frequency in order to avoid time aliasing effects.


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How to Cite
Kind, R. (1978). Extensions of the reflectivity method. Journal of Geophysics, 45(1), 373-380. Retrieved from https://journal.geophysicsjournal.com/JofG/article/view/174

References

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