Extrapolated supervirtual refraction interferometry

Extrapolated supervirtual refraction interferometry
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外推超虚拟折射干涉测量

DOI:
10.1093/gji/ggab283
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发表时间:
2021-08
影响因子:
2.8
通讯作者:
Liguo Han
Liguo Han
中科院分区:
地球科学2区
文献类型:
--
作者:
Zhuo Xu;Fengjiao Zhang;Christopher Juhlin;Bjorn Lund;Maria Ask;Liguo Han

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头波到达时间的准确选取是首到行时层析成像的重要组成部分。远偏移走线的信噪比(SNR)特别低,但为了获得深度的速度信息,必须对这些走线进行拾取。此外,为了在深度处获得可靠的模型,往往存在远偏移迹线的数量不足。我们在这里提出了一种外推方法来增加超过最大记录偏移量的第一次到达的数量,从而扩展了超虚拟折射干涉(SVI)方法。我们将这种方法称为外推SVI (ESVI)。这是一种利用完全数据驱动的方法来推断首次到达人数的新颖尝试。我们首先在合成数据集上测试方法,然后将ESVI应用于瑞典北部Pärvie断层系统上的两个已发布的真实数据集。这些数据集是在不同时间、不同采集参数和噪声水平下沿同一剖面采集的。结果表明,当噪声水平较高时,ESVI能提高头波的信噪比。这与传统的SVI相同。ESVI还通过外推头部波超过每次射击的原始最大偏移量来增加可选择的第一次到达的数量。我们还发现,首次到达时拾取的显著增加有利于提高层析成像的分辨率和穿透深度,从而更好地揭示地下速度分布。层析成像显示,相对于之前地震反射处理的偏移图像,主Pärvie断层和另一条辅助断层的上盘速度更高。
Accurate picking of head-wave arrival times is an important component of first-arrival traveltime tomography. Far-offset traces in particular have low signal-to-noise ratio (SNR), but picking on these traces is necessary in order to obtain velocity information at depth. Furthermore, there is often an insufficient number of far-offset traces for obtaining reliable models at depth. We present here an extrapolation method for increasing the number of first arrivals beyond the maximum recorded offset, thereby extending the supervirtual refraction interferometry (SVI) method. We refer to the method as extrapolated SVI (ESVI). It is a novel attempt to extrapolate first arrivals using a fully data-driven method. We first test the methodology on synthetic data sets, and we then apply ESVI to two published real data sets over the Pärvie fault system in northern Sweden. These data sets were acquired along the same profile at different times with different acquisition parameters and noise levels. The results show that ESVI enhances the SNR of head waves when the noise level is high. That is the same as the conventional SVI. ESVI also increases the number of pickable first arrivals by extrapolating head waves past the original maximum offset of each shot. We also show that the significant increase in first-arrival traveltime picks is beneficial for improving resolution and penetration depth in the tomographic imaging and, consequently, better revealing the subsurface velocity distribution. The tomographic images show higher velocities in the hanging walls of the main Pärvie fault and another subsidiary fault, as interpreted relative to migrated images from previous seismic reflection processing.
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发表时间: 2015-06
期刊: Solid Earth
影响因子: 3.4
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发表时间: 2020
期刊: Encyclopedia of Solid Earth Geophysics
影响因子: --
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DOI: 10.1190/geo2010-0039.1
发表时间: 2011-12
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影响因子: 3.3
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