초록 ▼

The present relates generally to the field of quantitative sedimentologic and stratigraphic prediction in which errors, uncertainties, risk and accuracy are calculated. Specifically, geologic data observed or inferred from core, outcrop, well log and/or seismic data from particular locations, in con

The present relates generally to the field of quantitative sedimentologic and stratigraphic prediction in which errors, uncertainties, risk and accuracy are calculated. Specifically, geologic data observed or inferred from core, outcrop, well log and/or seismic data from particular locations, in conjunction with a stratigraphic forward model and an optimization technique (mathematical inverse algorithm), are used to predict stratigraphic and sedimentologic attributes at locations other than those at which data were collected. This is accomplished by inverting a stratigraphic/sedimentologic forward model with simultaneous multi-parameter inversion or other mathematical optimization technique, such that forward model predictions are forced to obtain a best match with observations. The geologic data used to constrain the inversion are a small sample set of the larger, complete, rock volume simulated by the model.

대표청구항 ▼

[ What is claimed is:] [1.]1. A method for using geological data to predict one or more stratigraphic attributes at a location, the method comprising the steps of:obtaining real geological data from a location in a sedimentary basin;providing initial values to a stratigraphic forward model for param

[ What is claimed is:] [1.]1. A method for using geological data to predict one or more stratigraphic attributes at a location, the method comprising the steps of:obtaining real geological data from a location in a sedimentary basin;providing initial values to a stratigraphic forward model for parameters that are used by said stratigraphic forward model to output a predicted value for a stratigraphic attribute at said location at which said real geological data were obtained, wherein said forward model incorporates a conservation of mass constraint;using said stratigraphic forward model determine a predicted value for a stratigraphic attribute at said location at which real geological data were obtained based upon values of said parameters;determining a difference between said predicted value for said stratigraphic attribute and said real geological data at said location;modifying, if said difference does not satisfy a predetermined criteria, said values of said parameters to reduce said difference between said predicted value of said stratigraphic attribute and said real geological data;repeating said steps of using, determining and modifying until said difference satisfies said predetermined criteria; andidentifying, if said predetermined criteria is satisfied, said predicted value for said stratigraphic attribute as a best prediction for the actual value of the stratigraphic attributes over the space of the stratigraphic forward model.