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The most probable migration occurred along the network of fractures and faults planes Barrero et al. The Porquero Superior formation, composed of shales, presents a variable thickness and weak reflectors.
The seismic volume was processed up to a prestack migrated volume PSTM applying a special process sequence for AVO by angles range, the volume was interpreted as seen in the inline of Figure 2.
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The FCO has a variable thickness ranging from a few to meters with a m thickness average in the area. Theory The wave behavior at a discontinuity between two semi infinite elastic media is determined by the Zoeppritz equations, guaranteeing both displacement and stress continuity on the two opposite sides.
These equations were approximated by Shuey through the expression: According to equation 2 and in case of near offsets, i. In case of far offsets, i.
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After manipulating and solving them, the following is obtained: By using the equations 3 and 4, the Intercept and Gradient are correlated in a section, where the data located along the straight line defines the trend background whereas those others are orthogonally deviated to it Figure 4B. Although the shear velocity log was not acquired in this well, a pseudo shear velocity profile was calculated by the Greenberg-Castagna method The complete sets of logs, including the estimated pseudo shear log, are shown in figure 3A.
A well logs analysis in the m interval provided the following results. The GR log shows a sandstone-shale pattern. In depth, Poisson's relation log tends to decrease but arriving at the top of FCO gas reservoir at m it falls abruptly and rises immediately to continue its former decreasing trend. To match the seismic volume along the well, a synthetic seismogram was obtained by the convolution of a wavelet extracted from the seismic volume with the product of multiplying Sonic by Density logs, after depth to time conversion.
The Figure 3B depicts the stack section in the vicinity of the Ayombe-1 well along the - m interval. An obtained seismogram is seen in Figure 4Awhere amplitude is characterized by a positive intercept peak that decreases with an angle negative gradient at the top of the FCO fm.
The linear regression through data clustered in the upper polygon defines the background or the non anomalous data. The estimated straight line, with a slope of 1. The points which are not aligned with the background are considered anomalous, i. The Gamma Ray log remains unchanged because its response does not depend on fluids in pores. The Resistivity log falls quickly due to the gas is more resistive than water.
The Density log increases because water is denser than gas. The shear velocity remains the same because liquids cannot be sheared, whereas acoustic wave velocity increases due to the fact that liquids are not compressible.
Therefore, the top of the fully saturated water zone cannot be picked out. Besides, possible tuning related to absence of frequencies at far offsets might increase the uncertainty. Although, the near offset stack was not considered in this analysis because of the very low signal to noise ratio.