1887

Abstract

The field array is the group of seismic sensors connected to a single recording channel. The impact of field arrays on the spatial bandwidth of the recorded seismic data is described by the array wavenumber amplitude transfer function. In this paper, I discuss, however the impact of the field array on the temporal bandwidth of the recorded data. A requirement for this is an accurate knowledge of the field array geometry. I also propose a novel technique to correct the corresponding signal amplitude distortions in data processing.

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/content/papers/10.3997/2214-4609.20131230
2013-06-10
2021-10-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20131230
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