TY - GEN
T1 - Prestack first-break traveltime tomography using the double-square-root eikonal equation
AU - Li, Siwei
AU - Fomel, Sergey
AU - Vladimirsky, Alexander
N1 - KAUST Repository Item: Exported on 2020-10-01
Acknowledgements: The work was supported by Saudi Aramco and KAUST. Wethank Tariq Alkhalifah and Tim Keho for useful discussions.
This publication acknowledges KAUST support, but has no KAUST affiliated authors.
PY - 2012/10/25
Y1 - 2012/10/25
N2 - Traveltime tomography with shot-based eikonal equation fixes shot positions then relies on inversion to resolve any contradicting information between independent shots and achieve a possible cost-function minimum. On the other hand, the double-square-root (DSR) eikonal equation that describes the whole survey, while providing the same first-arrival travel-times, allows not only the receivers but also the shots to change position and therefore leads to faster convergence in tomo-graphic inversion. The DSR eikonal equation can be solved by a version of the fast-marching method (FMM) with special treatment for its singularity at horizontally traveling waves. For inversion, we use an upwind finite-difference scheme and the adjoint-state method to avoid explicit calculation of Fréchet derivatives. The proposed method generalizes to the 3D case straightforwardly.
AB - Traveltime tomography with shot-based eikonal equation fixes shot positions then relies on inversion to resolve any contradicting information between independent shots and achieve a possible cost-function minimum. On the other hand, the double-square-root (DSR) eikonal equation that describes the whole survey, while providing the same first-arrival travel-times, allows not only the receivers but also the shots to change position and therefore leads to faster convergence in tomo-graphic inversion. The DSR eikonal equation can be solved by a version of the fast-marching method (FMM) with special treatment for its singularity at horizontally traveling waves. For inversion, we use an upwind finite-difference scheme and the adjoint-state method to avoid explicit calculation of Fréchet derivatives. The proposed method generalizes to the 3D case straightforwardly.
UR - http://hdl.handle.net/10754/599396
UR - http://library.seg.org/doi/abs/10.1190/segam2012-0773.1
UR - http://www.scopus.com/inward/record.url?scp=85058096547&partnerID=8YFLogxK
U2 - 10.1190/segam2012-0773.1
DO - 10.1190/segam2012-0773.1
M3 - Conference contribution
SN - 9781622769452
SP - 4330
EP - 4335
BT - SEG Technical Program Expanded Abstracts 2012
PB - Society of Exploration Geophysicists
ER -