Abstract
The paper presents a general formula for the back projection of traveltime residuals in traveltime tomography. For special choices of an arbitrary weighting factor this formula reduces to the asymptotic back-projection term in ray-tracing tomography (RT), the Woodward-Rocca method, wavepath eikonal traveltime inversion (WET), and wave-equation traveltime inversion (WT). This unification provides for an understanding of the differences and similarities among these traveltime tomography methods. The special case of the WET formula leads to a computationally efficient inversion scheme in the space-time domain that is, in principle, almost as effective as WT inversion yet is an order of magnitude faster. -from Authors
Original language | English (US) |
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Pages (from-to) | 1314-1323 |
Number of pages | 10 |
Journal | Geophysics |
Volume | 58 |
Issue number | 9 |
DOIs | |
State | Published - 1993 |
Externally published | Yes |
ASJC Scopus subject areas
- Geochemistry and Petrology