作者:Xueyan Li,Yanbin Wang,Yongshun John Chen
摘要:The waveform inversion method is applied—using synthetic ocean-bottom seismometer(OBS) data—to study oceanic crust structure. A niching genetic algorithm(NGA) is used to implement the inversion for the thickness and P-wave velocity of each layer, and to update the model by minimizing the objective function, which consists of the misfit and cross-correlation of observed and synthetic waveforms. The influence of specific NGA method parameters is discussed, and suitable values are presented.The NGA method works well for various observation systems, such as those with irregular and sparse distribution of receivers as well as single receiver systems. A strategy is proposed to accelerate the convergence rate by a factor of five with no increase in computational complexity; this is achieved using a first inversion with several generations to impose a restriction on the preset range of each parameter and then conducting a second inversion with the new range. Despite the successes of this method,its usage is limited. A shallow water layer is not favored because the direct wave in water will suppress the useful reflection signals from the crust. A more precise calculation of the air-gun source signal should be considered in order to better simulate waveforms generated in realistic situations; further studies are required to investigate this issue.
發文機構:Department of Geophysics
關鍵詞:海底地震儀地殼結構反演方法OBS波形海洋小生境遺傳算法計算復雜度Waveform inversionOBSOceanic crustalstructureNiching genetic algorithm
分類號: P736.1[天文地球—海洋地質][天文地球—海洋科學]P315.2[天文地球—地震學][天文地球—固體地球物理學][天文地球—地球物理學]