A case study of TORT Q imaging of OBN data in a highly faulted area

Кейс-исследование Q-отрисовки по модели TORT для данных OBN в сильно разломленной области
Yiming Wang, Pin Zhang, Zaiyu Ding, T. J. Li, Jinlian Huang, Leilei Tian, J. Yan, Jianqing Guo, Tianjiu Zeng, Jinyu Guo, Lianbing Xie
2026-02-10

Ocean Bottom Node (OBN) wide-azimuth seismic dataTORT Q-compensation pre-stack depth migration (TORT Q-PSDM)imaging thin reservoirs and complex fault systemstilted orthorhombic anisotropy (TORT)velocity model building in highly faulted areas
In Ocean Bottom Node (OBN) wide-azimuth seismic data, especially in fracture-developed areas, challenges such as significant azimuthal anisotropy and insufficient accuracy in velocity model building persist. Traditional streamer seismic data, due to limited azimuthal coverage, is difficult to accurately characterize complex velocity models. Taking the WX area as an example, there are some difficulties in delineating low-order faults, uncertainties in fault combinations, velocity variations caused by deep-seated major faults, and imaging requirements for thin reservoirs. This paper is aimed to optimize velocity based on tilted orthorhombic anisotropic (TORT) model building and propose a technique that combines pre-stack depth migration and Q-compensation (TORT Q-PSDM). The focuses are on velocity model building and PSDM for OBN wide-azimuth data in complex fault areas and the application workflow. Results demonstrate that the workflow significantly improves imaging accuracy for complex fault systems, providing a reliable basis for subsequent exploration and development.
1
A workflow optimizing velocity with a tilted orthorhombic (TORT) anisotropic model and combining pre-stack depth migration with Q-compensation (TORT Q-PSDM) is proposed.
2
Application of the TORT Q-PSDM workflow in the WX area improves imaging accuracy for complex fault systems and thin reservoirs.
3
Improved imaging from the proposed workflow provides a more reliable basis for subsequent exploration and development in highly faulted areas.
4
OBN wide-azimuth seismic data in fracture-developed areas exhibits significant azimuthal anisotropy and challenges in accurate velocity model building.
5
Traditional streamer seismic data with limited azimuthal coverage cannot accurately characterize complex velocity models in highly faulted areas.

OBN (Ocean Bottom Node) wide-azimuth seismic data in a highly faulted (WX) area

Improving imaging accuracy via velocity model building using a tilted orthorhombic (TORT) anisotropy model and Q-compensated pre-stack depth migration (TORT Q-PSDM) for complex fault systems and thin reservoirs

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2026-02-10
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Yiming Wang
Pin Zhang
Zaiyu Ding
T. J. Li
Jinlian Huang
Leilei Tian
J. Yan
Jianqing Guo
Tianjiu Zeng
Jinyu Guo
Lianbing Xie
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