Source-receiver Marchenko redatuming: Obtaining virtual receivers and virtual sources in the subsurface

Author:

Singh Satyan1ORCID,Snieder Roel1

Affiliation:

1. Center for Wave Phenomena, Colorado School of Mines, Department of Geophysics, Golden, Colorado, USA..

Abstract

By solving the Marchenko equations, one can retrieve the Green’s function (Marchenko Green’s function) between a virtual receiver in the subsurface and points at the surface (no physical receiver is required at the virtual location). We extend the idea behind these equations to retrieve the Green’s function between any two points in the subsurface, i.e., between a virtual source and a virtual receiver (no physical source or physical receiver is required at either of these locations). This Green’s function is called the virtual Green’s function, and it includes all primary, internal, and free-surface multiples. Similar to the Marchenko Green’s function, this virtual Green’s function requires the reflection response at the surface (single-sided illumination) and an estimate of the first-arrival traveltime from the virtual locations to the surface. These Green’s functions can be used to image the interfaces from above and below.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Cited by 21 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Vertical Seismic-Profile Data Local Full-Waveform Inversion Based on Marchenko Redatuming;Applied Sciences;2023-03-24

2. Internal Multiple Removal and Illumination Correction for Seismic Imaging;IEEE Transactions on Geoscience and Remote Sensing;2022

3. Do we need up/down decomposition for Marchenko imaging?;First International Meeting for Applied Geoscience & Energy Expanded Abstracts;2021-09-01

4. Green’s function representations for Marchenko imaging without up/down decomposition;Geophysical Journal International;2021-06-07

5. Focusing waves in an unknown medium without wavefield decomposition;JASA Express Letters;2021-05

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