Tianfan Yan, Yike Liu, Zhendong Zhang, Bin He, Haiwei Wang
{"title":"Passive Sources and Diffracted Points Imaging Using Combinational Cross-Correlation Imaging Condition","authors":"Tianfan Yan, Yike Liu, Zhendong Zhang, Bin He, Haiwei Wang","doi":"10.1029/2024jb029695","DOIUrl":null,"url":null,"abstract":"Time-reversal imaging is a critical technique for characterizing natural earthquakes and artificial sources. Traditional time reversal methods sum the extrapolated wavefields of different receivers to suppress artifacts and obtain images of the sources. Multiplication-based time-reversal imaging uses the product of extrapolated wavefields to provide source images with fewer artifacts and higher resolutions. However, although multiplication among wavefields efficiently suppresses the artifacts, sources with weaker energy are also suppressed. We combined the two imaging algorithms and proposed a combinational cross-correlation reverse time migration (CcRTM) to image multiple sources. First, the receivers were divided into several groups and independently extrapolated in reverse time. Then, <i>n</i> receivers were selected each time, and the geometric mean between the receiver wavefields was calculated. In the third step, images of multiple sources were obtained using the arithmetic mean of all geometric mean results with different receiver combinations. Compared with multiplication-based source location methods, our method retains the root in the geometric mean to preserve the amplitude ratio between the sources. CcRTM can be applied to image diffractions by considering subsurface small-scale diffractors as secondary sources enabling the detection of anomalies smaller than the wavelength limit. To suppress the reflection energy, we introduced an excitation time to restrict the imaging time. Synthetic and field examples demonstrated the accuracy and efficiency of the proposed imaging method.","PeriodicalId":15864,"journal":{"name":"Journal of Geophysical Research: Solid Earth","volume":"27 1","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2025-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Solid Earth","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1029/2024jb029695","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Time-reversal imaging is a critical technique for characterizing natural earthquakes and artificial sources. Traditional time reversal methods sum the extrapolated wavefields of different receivers to suppress artifacts and obtain images of the sources. Multiplication-based time-reversal imaging uses the product of extrapolated wavefields to provide source images with fewer artifacts and higher resolutions. However, although multiplication among wavefields efficiently suppresses the artifacts, sources with weaker energy are also suppressed. We combined the two imaging algorithms and proposed a combinational cross-correlation reverse time migration (CcRTM) to image multiple sources. First, the receivers were divided into several groups and independently extrapolated in reverse time. Then, n receivers were selected each time, and the geometric mean between the receiver wavefields was calculated. In the third step, images of multiple sources were obtained using the arithmetic mean of all geometric mean results with different receiver combinations. Compared with multiplication-based source location methods, our method retains the root in the geometric mean to preserve the amplitude ratio between the sources. CcRTM can be applied to image diffractions by considering subsurface small-scale diffractors as secondary sources enabling the detection of anomalies smaller than the wavelength limit. To suppress the reflection energy, we introduced an excitation time to restrict the imaging time. Synthetic and field examples demonstrated the accuracy and efficiency of the proposed imaging method.
期刊介绍:
The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology.
JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields.
JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.