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On the effect of diffraction on traveltime measurements
Author(s) -
Gudmundsson 'Oli
Publication year - 1996
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1996.tb06372.x
Subject(s) - wavefront , fresnel zone , fresnel number , diffraction , fresnel diffraction , optics , waveform , perturbation (astronomy) , geology , physics , quantum mechanics , voltage
SUMMARY All observed waves are of finite frequency and are sensitive to a finite volume of the medium through which they pass. Diffraction causes a loss of information about time contained in the initial front of a wavefield (often referred to as wavefront healing). This effect depends upon frequency and propagation distance and imposes a low‐pass filter on the spatial resolution of time measurements. A sequence of canonical, numerical experiments that simulate the diffraction of a perturbed plane wave at a fixed distance is described. Traveltimes are measured using a variety of techniques on a range of waveforms. It is empirically verified that a single Fresnel zone describes the spatial filtering effect of the propagation of a broad‐band wavefield, even in the regime where the initial time perturbation cannot be represented by a linear perturbation term. For narrow‐band wavefields, more Fresnel zones come into play as the bandwidth is reduced. Measurements of time include a component of signal‐generated noise coherent over a small scale which scales with the Fresnel zone. It is found that, for traveltimes measured by automated picking, the width of the Fresnel zone is described by a time delay of |δ t | < T /4 (here T is one period). On the other hand, the width of the Fresnel zone for traveltimes measured by correlation is wider, characterized by a time delay of |δ t | < T /4.

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