Generation of Synthetic Seismograms for an Acoustic Layer over an Acoustic Half Space

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dc.contributor.authorFrazer, L. Neil
dc.date.accessioned2013-02-25T18:51:19Z
dc.date.available2013-02-25T18:51:19Z
dc.date.issued1981
dc.description.abstractThe problem of sound propagation in an acoustic layer over an acoustic half space (liquid over liquid) is solved by quadrature based on the generalized Filon method. Synthetic seismograms are computed by program NFAR1 for nearly arbitrary source-receiver distances and ranges of frequency. The user may optionally plot pressure and horizontal or vertical motion at specific distances. Test cases presented in the text demonstrate that the seismograms agree in arrival time and waveform for all anticipated events, such as direct, reflected, and refracted arrivals, including normal modes.en
dc.identifier.citationFrazer, L. Neil, 1981, Generation of Synthetic Seismograms for an Acoustic Layer over an Acoustic Half Space.Indiana Geological Survey Occasional Paper 35, 62 p., 9 fig.en
dc.identifier.urihttps://hdl.handle.net/2022/15306
dc.language.isoen_USen
dc.publisherIndiana Geological Surveyen
dc.relation.ispartofseriesOccasional Paper;35
dc.rightsThis work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/2.5/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA.en
dc.subjectSynthetic Seismograms, Acoustic Layer, Acoustic Half Space, Fortran IV Program NFAR1en
dc.titleGeneration of Synthetic Seismograms for an Acoustic Layer over an Acoustic Half Spaceen
dc.typeTechnical Reporten

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