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Method of generating 3-D geologic models incorporating geologic and geophysical constraints

Patent 5838634 Issued on November 17, 1998. Estimated Expiration Date: Icon_subject December 9, 2016. Estimated Expiration Date is calculated based on simple USPTO term provisions. It does not account for terminal disclaimers, term adjustments, failure to pay maintenance fees, or other factors which might affect the term of a patent.

Patent References

Method for seismic lithologic modeling
Patent #: 4679174
Issued on: 07/07/1987
Inventor: Gelfand

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Issued on: 08/28/1990
Inventor: Rimmer

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Issued on: 01/23/1996
Inventor: Neff

Method for deriving reservoir lithology and fluid content from pre-stack inversion of seismic data
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Issued on: 12/10/1996
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Seismic trace analysis method utilizing a statistical calibration technique for deducing geologic properties Patent #: 5638269
Issued on: 06/10/1997
Inventor: Fournier, et al.

Inventors

Application

No. 760951 filed on 12/09/1996

US Classes:

367/73, Synthetic seismograms and models702/12Fluid flow investigation

Examiners

Primary: Moskowitz, Nelson

Attorney, Agent or Firm

International Classes

G01V 001/34
G01V 001/30

Abstract

Features of subsurface earth reservoirs of interest are made available for analysis and evaluation by forming three-dimensional, geologic block models based on field data. The field data include geological observations, such as lithofacies and porosity values obtained from well data and other sources, as well as geophysical data, usually from seismic surveys. The geologic models representative of subsurface reservoirs so obtained are optimized to match as closely as feasible geologic constraints known or derived from observed geologic data. The models also conform to geophysically based constraints indicated by seismic survey data. The modeled geologic lithofacies and porosity are converted into acoustic velocity and bulk density values, which are then formulated as a seismic response which is then compared with actual seismic data. A perturbation process on lithofacies and porosity can be iteratively repeated until a representation of the reservoir is obtained which is within specified limits of accuracy or acceptability.

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