Passive Sources and Diffracted Points Imaging Using Combinational Cross-Correlation Imaging Condition

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Tianfan Yan, Yike Liu, Zhendong Zhang, Bin He, Haiwei Wang
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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.
利用组合互相关成像条件的被动光源和绕射点成像
时间反转成像是表征自然地震和人工震源的关键技术。传统的时间反演方法是将不同接收机的外推波场相加来抑制伪影,得到源的图像。基于乘法的时间反转成像使用外推波场的产物来提供具有更少伪影和更高分辨率的源图像。然而,虽然波场之间的倍增有效地抑制了伪影,但能量较弱的源也被抑制了。我们将两种成像算法结合起来,提出了一种组合互相关逆时偏移(CcRTM)对多源图像进行成像。首先,将受测者分成若干组,进行反向时间独立外推。然后,每次选取n个接收机,计算接收机波场之间的几何平均值。第三步,对不同接收机组合下的所有几何平均结果进行算术平均,得到多源图像。与基于乘法的源定位方法相比,我们的方法保留了几何平均值的根,以保持源之间的幅度比。CcRTM可以应用于图像衍射,通过考虑地下小规模衍射仪作为次要源,可以检测小于波长限制的异常。为了抑制反射能量,我们引入了激发时间来限制成像时间。综合和现场实例验证了该成像方法的准确性和有效性。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
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.
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