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Mode Theory versus Theoretical Seismograms for a Layered Solid
Author(s) -
Abramovici Flavian
Publication year - 1968
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1968.tb07131.x
Subject(s) - seismogram , mode (computer interface) , homogeneous , transfer function , geology , shear (geology) , frequency domain , continuation , mathematical analysis , physics , seismology , mathematics , statistical physics , computer science , petrology , engineering , electrical engineering , programming language , operating system
Spectral transfer functions are computed for a model consisting of one elastic layer over a homogeneous elastic half‐space. Represented in the time domain, the transfer functions are compared with theoretical seismograms for various horizontal distances. The diagnostic diagrams show that the P̄ +‐ ‐mode, the contribution of which is important in the generation of the PL ‐waves, is not the continuation of the first locked shear mode below the cut‐off frequency.

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