SEG Technical Program Expanded Abstracts 2004 2004
DOI: 10.1190/1.1851132
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What seismic velocity field for pore pressure prediction?

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Cited by 5 publications
(5 citation statements)
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“…The choice of the attribute to use depends on many factors, as the complexity of the area under study in terms both of structure and pressure regime, data and time available to perform the study and of course the costs required to carry out it. (Cibin P. et al 2004) With Continuous Velocity Analysis (CVA) technique a very dense and detailed velocity field can be generated starting from the PSTM velocities elaborated during the time processing. Each gather is stacked after NMO correction with many trial functions and the stacked traces are scanned to find the highest amplitude at every time sample.…”
Section: Discussionmentioning
confidence: 99%
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“…The choice of the attribute to use depends on many factors, as the complexity of the area under study in terms both of structure and pressure regime, data and time available to perform the study and of course the costs required to carry out it. (Cibin P. et al 2004) With Continuous Velocity Analysis (CVA) technique a very dense and detailed velocity field can be generated starting from the PSTM velocities elaborated during the time processing. Each gather is stacked after NMO correction with many trial functions and the stacked traces are scanned to find the highest amplitude at every time sample.…”
Section: Discussionmentioning
confidence: 99%
“…The Grid Tomography is based on ray tracing techniques to compute the residual moveouts and takes information not only from geological consistent reflecting horizons, but also from local events, seismically coherent, interpretable just in restricted areas of the model. Also in this case, the possibility to depart from a definite horizons based model using further information from extra seismic events, gives the opportunity to highlight velocity anomalies in the updated velocity field often associated to pore pressure anomalies (Cibin P.2006, 2008, 2010and Colin Sayers, 2000.…”
Section: Discussionmentioning
confidence: 99%
“…Both velocities can be used quite successfully where the theoretical conditions for the application of Dix equation are valid. With Continuous Velocity Analysis (CVA) techniques, the PSTM velocities are used as initial reference functions in a refining process giving a very dense and detailed velocity field as output and generating a pore pressure field that can highlight over pressure anomalies in not too much complex areas [Cibin P., (2004)]. …”
Section: Methodsmentioning
confidence: 99%
“…Once all the terms of Eaton formula are defined, the seismic interval velocities cube can be converted into effective stress cube. At the end of the process, the pore pressure volume is obtained by subtracting the effective stress volume to the overburden volume and then the overpressure volume is calculated as difference between the pore pressure volume and the hydrostatic pressure volume [Cibin P., (2008)]. …”
Section: Methodsmentioning
confidence: 99%
“…As part of the seismic processing work-flow, several velocity models can be derived ranging from simple normal-moveout to tomographic inversion and more recently to full-wave inversion. The choice of which to use depends on the complexity of the problem (Cibin et al, 2004).…”
mentioning
confidence: 99%