Abstract
Two new techniques are presented for the inversion of first-arrival times to estimate velocity structure. These travel-time inversion techniques are unique in that they do not require the calculation of ray paths. First-arrival times are calculated using a finite-difference scheme that iteratively solves the eikonal equations for the position of the wavefront. The first inversion technique is a direct extension of linearized waveform inversion schemes. The nonlinear relationship between the observed first-arrival times and the model slowness is linearized using a Taylor series expansion and a solution is found by iteration. For a series of two-dimensional numerical tests, with and without random noise, this travel-time inversion procedure accurately reconstructed the synthetic test models. The second inversion technique is an application of simulated annealing to travel-time topography. The linearized inversion scheme outperforms the nonlinear simulated annealing approach. -from Authors
Original language | English (US) |
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Pages (from-to) | 509-528 |
Number of pages | 20 |
Journal | Bulletin - Seismological Society of America |
Volume | 83 |
Issue number | 2 |
State | Published - 1993 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology