--> ABSTRACT: A Case Study on Using Seismic Inversion, 90 Degree Phase Shifted Seismic Data and Geostatistical Simulation in the Bayu-Undan Field, by Joseph Gallagher, M. J. Raymondi, and D. Mayo; #90913(2000).
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ABSTRACT: A case study on using Previous HitseismicNext Hit Previous HitinversionNext Hit, 90 degree phase shifted Previous HitseismicNext Hit Previous HitdataNext Hit and geostatistical simulation in the Bayu-Undan Field

Gallagher, Joseph, M. J. Raymondi, and D. Mayo , Phillips Petroleum Co, Bartlesville, OK

A measure of the impedance variation can be obtained Previous HitfromNext Hit the negative first derivative of the Previous HitseismicNext Hit trace or by applying to the zero phase Previous HitseismicNext Hit section, a phase shift of -90 degrees. In this paper, it is shown that this process can provide a quantitative measure of the high and low values of impedance along a Previous HitseismicNext Hit trace. Peaks on Previous HitseismicNext Hit trace processed in this way can be associated with intervals of increases in impedance while toughs on the trace can be associated with intervals of decreases in impedance. Previous HitSeismicNext Hit sections processed in this manner are compared to a sparse spike geostatistical-based Previous HitinversionNext Hit performed on the Previous Hit3-DNext Hit Previous HitseismicNext Hit Previous HitdataNext Hit acquired over the Bayu-Undan field in the Timor Sea. The Previous HitinversionNext Hit encompassed the entire reservoir interval. Sonic and density logs Previous HitfromNext Hit seven wells were used to geostatistically build a low frequency impedance model and an amplitude balance model. These models were Previous HitappliedNext Hit to the sparse spike Previous HitinversionNext Hit in the frequency domain to generate absolute impedances for the inverted Previous HitseismicNext Hit traces. Previous HitFromNext Hit the impedance and -90 phase shifted Previous HitseismicNext Hit section and using gamma ray log calibration, it is shown that peaks in the Previous HitseismicNext Hit trace are associated with higher impedance values and shale intervals while troughs are associated with lower impedance and sand intervals. The estimation of porosity in the sands using impedance/porosity correlation as soft Previous HitdataTop in a geostatistical simulation are also discussed.

AAPG Search and Discovery Article #90913©2000 AAPG International Conference and Exhibition, Bali, Indonesia