z-logo
open-access-imgOpen Access
Resolution limit of traveltime tomography
Author(s) -
Dahlen F. A.
Publication year - 2004
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.2004.02214.x
Subject(s) - slowness , cube root , amplitude , seismic tomography , wavefront , diffraction , geology , seismology , tomography , geodesy , cube (algebra) , limit (mathematics) , seismic wave , mathematical analysis , mathematics , physics , optics , geometry
SUMMARY We derive an explicit formula relating a recovered 3‐D seismic slowness image to the actual seismic slowness under the assumption that a tomographically complete collection of finite‐frequency traveltime shifts is inverted using linearized ray theory. The tomographically recovered image is blunted, or diminished in amplitude, and blurred, or spread laterally, as a result of wave front healing and other finite‐frequency diffraction effects. The 1‐D spreading varies as the cube root of the amplitude reduction, so that total volume‐integrated slowness is conserved.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here