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Acoustic wave-equation traveltime and waveform inversion of crosshole seismic data

Journal Article · · Geophysics
DOI:https://doi.org/10.1190/1.1443815· OSTI ID:87546
; ; ;  [1];  [2]
  1. Univ. of Utah, Salt Lake City, UT (United States). Dept. of Geology and Geophysics
  2. Sun Microsystems Computer Corp., Mountain view, CA (United States)

A hybrid wave-equation traveltime and waveform inversion method is presented that reconstructs the interwell velocity distribution from crosshole seismic data. This inversion method, designated as WTW, retains the advantages of both full wave inversion and traveltime inversion; i.e., it is characterized by reasonably fast convergence which is somewhat independent of the initial model, and it can resolve detailed features of the velocity model. In principle, no traveltime picking is required and the computational cost of the WTW method is about the same as that for full wave inversion. The authors apply the WTW method to synthetic data and field crosshole data collected by Exxon at their Friendswood, Texas, test site. Results show that the WTW tomograms are much richer in structural information relative to the traveltime tomograms. Subtle structural features in the WTW Friendswood tomogram are resolved to a spatial resolution of about 1.5 m, yet are smeared or completely absent in the traveltime tomogram. This suggests tat it might be better to obtain high quality (distinct reflections) crosshole data at intermediate frequencies, compared to intermediate quality data (good quality first arrivals, but the reflections are buried in noise) at high frequencies.

OSTI ID:
87546
Journal Information:
Geophysics, Journal Name: Geophysics Journal Issue: 3 Vol. 60; ISSN GPYSA7; ISSN 0016-8033
Country of Publication:
United States
Language:
English