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CHAPTER 6




                            INTEGRATION

                           WITH SEISMIC










            While one part of petrophysics is concerned with the interface with geol-
            ogists and reservoir engineers in order to produce reservoir models, a
            further interface exists with the seismologists to ensure that the well data
            are used to help calibrate and understand seismic properties.
               While the preparation of synthetic seismograms to tie log-formation
            tops with seismic horizons is a long-established technique, recent ad-
            vances in far-offset seismic processing, combined with the ability to
            measure shear-sonic transit times, have opened up a lot of new possibili-
            ties for facies and fluid determination from seismic data. In this chapter
            some of these techniques will be discussed.

                           6.1 SYNTHETIC SEISMOGRAMS


               There are two elements to synthetic seismograms. The first is the der-
            ivation of the acoustic impedance (AI) from the log data, from which
            reflectivity may be derived. The second is the conversion of the depth-
            related traces from a depth reference to a time reference so they can be
            compared with seismic sections. From the log data, the following may be
            derived:

               V p = 1 6  (3 281 sonic,  *  )                          (6.1.1)
                    e
            where V p is in m/s and sonic is measured in ms/ft.

               r= 1e6*density                                          (6.1.2)


                             3
            where r is in kg/m and density is measured in g/cc.


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