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A FRACTAL-BASED ALGORITHM FOR DETECTING FIRST ARRIVALS ON SEISMIC TRACES

机译:基于分形的地震道首次探测算法

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A new algorithm is proposed for the automatic picking of seismic first arrivals that detects the presence of a signal by analyzing the variation in fractal dimension along the trace. The ''divider-method'' is found to be the most suitable method for calculating the fractal dimension. A change in dimension is found to occur close to the transition from noise to signal plus noise, that is the first arrival. The nature of this change varies from trace to trace, but a detectable change is always found to occur. The algorithm has been tested on real data sets with varying SIN ratios and the results compared to those obtained using previously published algorithms. With an appropriate tuning of its parameters, the fractal-based algorithm proved more accurate than all these other algorithms, especially in the presence of significant noise. The fractal method proved able to tolerate noise up to 80% of the average signal amplitude. However: the fractal-based algorithm is considerably slower than the other methods and hence is intended for use only on data sets with low SIN ratios. [References: 22]
机译:提出了一种自动提取地震初次到达的新算法,该算法通过分析沿轨迹的分形维数的变化来检测信号的存在。发现“除法”是最适合计算分形维数的方法。发现尺寸变化发生在从噪声到信号加噪声的过渡附近,即首次到达。这种变化的性质因迹而异,但是总是发现可检测到的变化发生。该算法已在具有不同SIN比率的真实数据集上进行了测试,并将结果与​​使用以前发布的算法获得的结果进行了比较。通过适当调整其参数,基于分形的算法被证明比所有其他算法更准确,尤其是在存在明显噪声的情况下。分形方法证明能够承受高达平均信号幅度80%的噪声。但是:基于分形的算法比其他方法要慢得多,因此只能用于具有低SIN比率的数据集。 [参考:22]

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