Data merging methods for S-wave velocity and azimuthal anisotropy from different regions

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Abstract

When inverting the S-wave velocity and azimuthal anisotropy from ambient noise data, it is always to obtain the partial overlapped inversion results in contiguous different regions. Merging different data to achieve a consistent model becomes an essential requirement. Based on the S-wave velocity and azimuthal anisotropy obtained from different contiguous regions, this paper introduces three kinds of methods for merging data. For data from different regions with partial overlapping areas, the merged results could be calculated by direct average weighting (DAW), linear dynamic weighting (LDW), and Gaussian function weighting (GFW), respectively. Data tests demonstrate that the LDW and GFW methods can effectively merge data by reasonably allocating data weights to capitalize on the data quality advantages in each zone. In particular, they can resolve the data smoothness at the boundaries of data areas, resulting in a consistent data model in larger regions. This paper presents the effective methods and valuable experiences that can be referred to as advancing data merging technology.
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不同区域 S 波速度和方位各向异性的数据合并方法
从环境噪声数据反演 S 波速度和方位各向异性时,总是要在连续的不同区域获得部分重叠的反演结果。合并不同数据以获得一致的模型成为一项基本要求。基于从不同连续区域获得的 S 波速度和方位各向异性,本文介绍了三种合并数据的方法。对于部分重叠区域的不同区域数据,可分别采用直接平均加权法(DAW)、线性动态加权法(LDW)和高斯函数加权法(GFW)计算合并结果。数据测试表明,线性动态加权法和高斯函数加权法通过合理分配数据权重,充分利用各区的数据质量优势,可以有效地合并数据。特别是,它们可以解决数据区域边界的数据平滑问题,从而在更大的区域内形成一致的数据模型。本文介绍了这些有效的方法和宝贵的经验,可谓数据合并技术的进步。
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Site classification methodology using support vector machine: A study Improving image accuracy of ambient noise data by temporary seismic arrays at different observation periods Data merging methods for S-wave velocity and azimuthal anisotropy from different regions Characterization and application of submarine seismic ambient noise in the Bohai Sea and Yellow Sea Rapid determination of source parameters of the M6.2 Jishishan earthquake in Gansu Province and its application in emergency response
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