Topography-dependent eikonal tomography based on the fast-sweeping scheme and the adjoint-state technique

Author:

Guo Gaoshan1ORCID,Lan Haiqiang2ORCID,Zhou Xiaole1ORCID,Liu Youshan1ORCID,Bin Waheed Umair3,Chen Jingyi4

Affiliation:

1. Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Beijing 100029, China and University of Chinese Academy of Sciences, Beijing 100049, China.

2. Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Beijing 100029, China and University of Chinese Academy of Sciences, Beijing 100049, China. (corresponding author)

3. King Fahd University of Petroleum and Minerals, College of Petroleum Engineering and Geosciences, Dhahran 31261, Saudi Arabia.

4. The University of Tulsa, Department of Geosciences, Tulsa, Oklahoma 74104-9700, USA.

Abstract

First-arrival traveltime tomography has been widely used for upper crustal velocity modeling, but it usually suffers from the problem of complex surface topography. To overcome this problem, we have developed a new topography-dependent eikonal tomography scheme that combines a developed accurate and efficient traveltime modeling method and introduces a flexible and robust adjoint inversion scheme in the presence of irregular topography. A surface-flattening scheme is used to handle the irregular surface, where the real model is discretized by curvilinear grids and the irregular free surface is mathematically flattened through the transformation from Cartesian to curvilinear coordinates. Based on this parameterization, the forward traveltime modeling is conducted by a monotone fast-sweeping method that discretizes the factored topography-dependent eikonal equation with a point-source condition. This algorithm can circumvent the source-singularity problem and decrease the numerical error in the vicinity of a point source in the curvilinear system. Then, the gradient-based inversion is used to minimize the misfit function, which is achieved by a matrix-free adjoint-state method without cumbersome ray tracing and explicit estimation of the Fréchet derivative matrix in the curvilinear coordinate system. The new tomographic scheme is evaluated through numerical examples with different seismic structures with complex topography, and then applied to a wide-angle profile acquired in the northeastern Tibetan Plateau. The results validate the effectiveness and efficiency of our tomography scheme in constructing shallow crustal velocity models with irregular topography.

Funder

National Natural Science Foundation of China

the Open Fund Project State Key Laboratory of Lithospheric Evolution

the Strategic Priority Research Program

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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