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首页> 外文期刊>Journal of environmental & engineering geophysics >Genetic algorithm inversion of Rayleigh wave dispersion from CMPCC gathers over a shallow fault model
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Genetic algorithm inversion of Rayleigh wave dispersion from CMPCC gathers over a shallow fault model

机译:CMPCC瑞利波频散的遗传算法反演在浅层断层模型上聚集

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Lateral shear-wave velocity imaging, based on 1D surface wave inversion, is becoming routine in commercial site characterisation. A Genetic Algorithm (GA) is applied to the inversion of fundamental mode Rayleigh wave dispersion over a 3-layered, shallow, vertical-fault model. The data are calculated using a 2D finite difference method, then sorted into CMP cross-correlated (CMPCC) gathers, from which the dispersion is measured. Dispersion is relatively smooth over flat portions of the model, as well as when the spread is equally centered over the sharp lateral discontinuity. When between one and two-fifths of the spread is "overhanging" the fault, low-frequency dispersion is corrupted by wavefield scattering. Each dispersion curve is inverted using a 1D forward model, constrained to four layers, with parameters allowed to vary within liberal limits except the layer 1 shear-wave velocity. A novel variation is that the optimisation is partially directed, by
机译:基于一维表面波反演的横向剪切波速度成像在商业现场表征中已成为常规。将遗传算法(GA)应用于三层浅浅垂直故障模型上的基本模式瑞利波频散的反演。使用2D有限差分法计算数据,然后将其分类为CMP互相关(CMPCC)道集,从中测量离散度。色散在模型的平坦部分上相对平滑,并且当色散在尖锐的横向不连续点上均等地居中时。当扩展的五分之一到五分之二“悬垂”于断层时,低频色散会被波场散射破坏。使用一维正向模型将每个频散曲线反转,并限制为四层,其中参数允许在第1层剪切波速度以外的自由范围内变化。一种新颖的变化是,优化是通过

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