Receiver-side near-surface corrections in the τ-p domain: A raypath-consistent solution for converted wave processing
| Autor: | Raul Cova, Xiucheng Wei, Kristopher A. Innanen, David C. Henley |
|---|---|
| Rok vydání: | 2017 |
| Předmět: |
Surface (mathematics)
010504 meteorology & atmospheric sciences business.industry Mathematical analysis 010502 geochemistry & geophysics 01 natural sciences Domain (mathematical analysis) Geophysics Optics Geochemistry and Petrology Consistency (statistics) S-wave Constant (mathematics) business Statics Energy (signal processing) 0105 earth and related environmental sciences Mathematics |
| Zdroj: | GEOPHYSICS. 82:U13-U23 |
| ISSN: | 1942-2156 0016-8033 |
| DOI: | 10.1190/geo2016-0278.1 |
| Popis: | Removing near-surface effects in the processing of 3C data is key to exploiting the information provided by converted waves. Particularly for the case of the PS-mode, converted energy travels back to the surface as S-waves. Therefore, S-wave static corrections are needed for the receiver side. This is often done under the assumption of surface consistency. This implies a constant correction for all the traces recorded at a fixed receiver location. However, if the velocity change between the near-surface layer and the medium underneath is gradual, the vertical raypath assumption that supports the surface-consistent approach is no longer valid. This property results in a nonstationary change of the near-surface traveltimes that need to be addressed to properly solve the problem. We have determined how the delays introduced by the presence of very low S-wave velocities in the near surface can introduce raypath-dependent effects. The magnitudes of these delays can be larger than what can be considered a residual static. In this study, a raypath-consistent approach is used to solve the problem. This is achieved by transforming the data, organized into receiver gathers, to the [Formula: see text]-[Formula: see text] domain and performing crosscorrelation and convolution operations to capture and remove the near-surface delays from the data. We tested this processing technique on synthetic and field data. In both cases, removing near-surface time delays in a raypath-consistent framework improved the coherency and stacking power of shallow and deep events simultaneously. Shallow events benefited most from this processing due to their wider range of reflection angles. This approach can be useful in the processing of wide-angle broadband data in which the kinematics of wave propagation are not consistent with vertical raypath approximations in the near surface. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|