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Repeatability in geophysical data processing: A case study of seismic refraction tomography

机译:地球物理数据处理中的可重复性:以地震折射层析成像为例

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This research work was carried out to determine the extent to which a geophysical data could give similar results (anomalies) when reprocessed under the same condition. Hence seismic refraction tomography processing which depends on picked arrival times was carried out to ascertain this fact. The processing flow started from importing raw seismic data, down to generation of the tomography model that represent the distribution of seismic velocities within the subsurface. Each of the two different raw seismic data collected from two profiles was reprocessed for three times, under the same condition, using the same software. The major factor that naturally varied during the data processing was the picked first arrival travel times. The results showed similar velocity distribution within the subsurface in each of the three models, that is, areas of low velocities corresponding with areas of low velocities and vies versa. The average thickness of the overburden and depth to basement appeared to be the same in all the tomographic models. However, subtle features like the subsurface geometry and basement topography did not show much similarity in appearance. It was concluded that geophysical data should be processed at least three times along with other constrain, and the extent of repeatability observed, before any meaningful interpretation can be drawn from it. This has also revealed that in the event of time laps investigation, geophysical data should be reprocessed several times to ensure that the observed changes are not due to processing artefact, rather that geological changes.
机译:进行这项研究工作是为了确定在相同条件下进行重新处理时,地球物理数据在多大程度上可以给出相似的结果(异常)。因此,进行了取决于所选择的到达时间的地震折射层析成像处理来确定这一事实。处理流程从导入原始地震数据开始,一直到生成代表地下地下地震速度分布的层析成像模型。在相同条件下,使用相同软件,将从两个剖面收集的两个不同原始地震数据中的每个数据进行了三次处理。在数据处理过程中自然变化的主要因素是所选择的首次到达旅行时间。结果表明,在这三个模型中,每个模型的地下速度分布相似,即低速区域对应于低速区域,反之亦然。在所有层析成像模型中,表层的平均厚度和至基底的深度似乎都相同。但是,诸如地下几何形状和地下室地形之类的细微特征在外观上并未显示出太多相似之处。得出的结论是,在可以从中得出任何有意义的解释之前,地球物理数据应与其他约束条件一起至少处理三遍,并观察可重复性的程度。这也表明,在进行时间间隔调查的情况下,应该对地球物理数据进行多次处理,以确保观察到的变化不是由于处理伪影,而是由于地质变化。

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