Seismic impedance inversion and interpretation of a gas carbonate reservoir in the Alberta Foothills, western Canada

Author:

Madiba Gislain B.1,McMechan George A.1

Affiliation:

1. University of Texas at Dallas, Center for Lithospheric Studies, P.O. Box 830688 (FA31), Richardson, Texas 75083‐0688. Emails:

Abstract

Acoustic and simultaneous elastic impedance inversions of a 2D land seismic data set are performed to characterize a carbonate reservoir of Mississippian age in the Turner Valley Formation, in the Rocky Mountain foothills of western Canada. The inversions produce P‐wave and S‐wave impedance sections (Ipand Is, respectively), from which Lamé parameter × density (λρ and μρ) sections are derived. The Ipdata provide a separation between the clastics and carbonates. The μρ data provide an estimate of porosity distribution within the dolomitized limestone target. Deviations from baseline curves for water‐saturated carbonates, of λρ versus porosity, λ/μ versus porosity, and Isversus Ip, are interpreted as indicators of gas potential. These indicators all provide similar spatial patterns of areas of high gas potential and are consistent with the gas occurence observed in a well.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference41 articles.

1. Al‐Aasm, I. S., and Lu, F., 1994, Multistage dolomitization of the Mississippian Turner Valley Formation, Quirk Creek Field, Alberta; chemical and petrologic evidence,inGlass, D. J., Beauchamp, B., and Embry, A. F., Eds., Pangea: Global environments and resources: Can. Soc. Petr. Geol. Memoir17, 657–675.

2. Anno, P. D., 1985, Exploration of the Hunton group, Anadarko Basin, using shear waves: 55th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 345–348.

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