Elastic reverse time migration angle gathers using a stabilized Poynting vector without zero points within the wave propagation ranges

Author:

Yang Kai1ORCID,Wang Xiaoyi2ORCID,Zhang Jianfeng3

Affiliation:

1. Southern University of Science and Technology, Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology, Shenzhen, China and Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China.

2. Chinese Academy of Sciences, Institute of Geology and Geophysics, Key Laboratory of Petroleum Resources Research, Beijing, China.

3. Southern University of Science and Technology, Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology, Shenzhen, China and Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China. (corresponding author)

Abstract

Generation of PP and PS angle gathers for elastic reverse time migration (ERTM) has important applications in velocity model updating and subsurface parameter inversion. The Poynting-vector-based method provides a cost-effective way to extract angle gathers from ERTM. However, the estimated propagation directions or angles based on Poynting vectors at or near zero points are unstable, and the reflection energy at these points is likely to be placed in an incorrect angle bin. This instability problem severely limits its use in the generation of high-quality angle gathers. To overcome this problem, we add the conventional Poynting vector with an ancillary one of the Hilbert transformed wavefield, a 90° phase-shifted version of the original wavefield. The Poynting vector of the Hilbert transformed wavefield points in the same propagation direction as the conventional Poynting vector, but they have different zero-point distributions. Adding them together allows us to obtain a stabilized Poynting vector which thoroughly eliminates the zero points within the wave propagation range, and thus we obtain a stable algorithm to extract high-quality angle gathers from ERTM. The Hilbert transformed wavefield already exists in the P/S and up/down wavefield decomposition procedure, which has become a necessary step for ERTM to separate overlapping wavefields at reflectors before the computation of Poynting vectors. Results from two synthetic numerical examples indicate the effectiveness of our method in generating high-quality angle gathers for ERTM.

Funder

National Natural Science Foundation of China

Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology

National Key RD Program of China

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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