Page 220 - Acquisition and Processing of Marine Seismic Data
P. 220

CHAPTER

                                                     4





                    Fundamentals of Data Processing












                                               OUTLINE

              4.1 Autocorrelation                 213    4.6 2D Fourier Transform             222
              4.2 Crosscorrelation                215    4.7 z Transform                      230
              4.3 Convolution                     215    4.8 Hilbert Transform                231

              4.4 Fourier Series                  216    4.9 τ-p Transform (Slant Stack)      232
              4.5 1D Fourier Transform            219   4.10 Sampling Theory                  235



              In seismic data processing, some fundamental  such as auto- and cross-correlations and convolu-
           processes and the determination of processing  tion, some generalized functions such as the
           parameters are accomplished by analyzing spe-  Dirac Delta or unit impulse, box-car or sinc func-
           cific correlation functions and frequency compo-  tion, and some of the most common transforms
           nents of the input seismic data. Correlation can be  such as the Fourier, Hilbert or τ-p transforms
           handled by computing auto- or cross-correlation  and their characteristics, as well as application
           functions, while the frequency characteristics of  fields, are explained.
           the data are investigated by computing the Fou-  Signal processing in geophysics is generally
           rier transform, which moves the data from the  achieved by carrying out a number of mathe-
           time to the frequency domain. In addition, some  matical processes applied to the geophysical sig-
           of the processing steps such as bandpass filtering  nal, which is generally in the form of discrete
           or deconvolution in the time domain are imple-  time series. Based on the environment where
           mented by convolution. Since these applications  the signal is observed, the data is a function of
           are the main tools of data processing, their funda-  either time or space: that is, the data is defined
           mental concepts and basic properties have signif-  in time or distance domains, respectively. If
           icant importance for a seismic processor. In this  the observed signal is a function of frequency,
           section, some of the basic mathematical processes  then the frequency domain is considered. It is



           Acquisition and Processing of Marine Seismic Data  211             # 2018 Elsevier Inc. All rights reserved.
           https://doi.org/10.1016/B978-0-12-811490-2.00004-9
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