Systems and methods for building axes, co-axes and paleo-geographic coordinates related to a stratified geological volume
View Patent ↗A method and system for modeling a subsurface structure at a time when the structure was originally formed. A first model having non-planar horizons representing a current subsurface structure may be used to calculate a vector field based on the non-planar geometry of the horizons of the model. The vector field may be non-uniform or uniform. Geographic coordinates of the first model may be transformed to paleo-geographic coordinates of a model representing the subsurface structure in the past, where the non-planar horizons in the first model are transformed to planar horizons in the second model. A set of points describing one or more fractures in the subsurface structure may be used to calculate a tuning parameter to correct a first set of paleo-geographic coordinates. A second set of coordinates representing an improved prediction at a time period when the subsurface structure was originally formed may be generated.
1. A method for modeling a subsurface structure at a time period when the structure was originally formed, comprising:
generating a first set of paleo-geographic coordinates representing a predicted state of the subsurface structure at a time period when the subsurface structure was originally formed;
defining a set of points describing one or more fractures in the subsurface structure;
determining, based on the defined set of points, at least one tuning parameter to correct the first set of paleo-geographic coordinates that minimizes discrepancy between an estimated direction of potential fracture and an observed direction of fracture;
generating, based on the at least one tuning parameter, a second set of paleo-geographic coordinates representing an improved predicted state of the subsurface structure at a time period when the subsurface structure was originally formed; and
displaying a visualization of the second set of paleo-geographic coordinates representing the improved predicted state of the subsurface structure.
2. The method of claim 1 , wherein the one or more fractures are observed in the subsurface structure in a current state.
3. The method of claim 1 , wherein the estimated direction of potential fracture is a strain tensor describing the relationship between the first set of paleo-geographic coordinates and a current state of the subsurface structure.
4. The method of claim 1 , wherein determining at least one tuning parameter comprises, for each of the points describing one or more fractures, determining a tuning value that minimizes discrepancy between the estimated direction of potential fracture and the observed direction of fracture at the point of fracture.
5. The method of claim 4 , wherein determining at least one tuning parameter comprises determining the mean or median of the determined tuning values.
6. The method of claim 1 , wherein the at least one tuning parameter is a constant.
7. The method of claim 1 , wherein the at least one tuning parameter is a function of geographic coordinates.
8. The method of claim 1 , wherein generating a second set of paleo-geographic coordinates comprises transforming the first set of paleo-geographic coordinates according to a Galilean transformation.
9. The method of claim 1 , wherein generating a second set of paleo-geographic coordinates comprises transforming the first set of paleo-geographic coordinates according to a shear transformation.
10. A system configured to model a subsurface structure at a time period when the structure was originally formed, the system comprising:
a memory configured to store set of points describing one or more fractures in the subsurface structure;
a processor configured to:
generate a first set of paleo-geographic coordinates representing a predicted state of the subsurface structure at a time period when the subsurface structure was originally formed;
determine, based the set of points, at least one tuning parameter to correct the first set of paleo-geographic coordinates that minimizes discrepancy between an estimated direction of potential fracture and an observed direction of fracture;
generate, based on the at least one tuning parameter, a second set of paleo-geographic coordinates representing an improved predicted state of the subsurface structure at a time period when the subsurface structure was originally formed; and
display a visualization of the second set of paleo-geographic coordinates representing the improved predicted state of the subsurface structure.
11. The system of claim 10 , wherein
the memory is configured to:
store a model having a plurality of non-planar horizons representing a current state of the subsurface structure; and
the processor is configured to generate the first set of paleo-geographic coordinates by:
computing a non-uniform vector field based on the non-planar geometry of the horizons of the model and
transforming geographic coordinates of the model to paleo-geographic coordinates representing a predicted state of the subsurface structure at a time period when the subsurface structure was originally formed, wherein the non-planar horizons in the model are transformed to planar horizons in the first set of paleo-geographic coordinates.
12. The system of claim 10 , wherein the processor is configured to determine at least one tuning parameter, by determining, for each of the points describing one or more fractures, a tuning value that minimizes discrepancy between the estimated direction of potential fracture and the observed direction of fracture at a point of fracture.
13. The system of claim 10 , wherein the estimated direction of potential fracture is a strain tensor describing the relationship between the first set of paleo-geographic coordinates and a current state of the subsurface structure.
14. The system of claim 10 , where the processor is configured to determine at least one tuning parameter by determining a mean or median of the determined tuning values.
15. The system of claim 10 , wherein the processor is configured to generate a second set of paleo-geographic coordinates by transforming the first set of paleo-geographic coordinates according to a Galilean, shearing, or other geometric transformation.
16. A method for modeling a subsurface structure, comprising:
generating a first model having a plurality of non-planar horizons representing a current state of the subsurface structure;
transforming geographic coordinates of the first model to paleo-geographic coordinates of a second model representing a predicted state of the subsurface structure at a time period when the subsurface structure was originally formed,
defining a model of one or more observed fractures in the current state of the subsurface structure
determining tuning parameters minimizing discrepancy between an estimated direction of potential fracture and an observed direction of the one or more observed fractures; and
using the tuning parameters, generating a third model representing an improved predicted state of the subsurface structure at a time period when the subsurface structure was originally formed; and
displaying a visualization of the third model representing the improved predicted state of the subsurface structure.
17. The method of claim 16 , wherein generating a third model comprises transforming paleo-geographic coordinates of the second model to minimize discrepancy between an estimated strain tensor between the second model and the first model and an observed direction of fracture.
18. The method of claim 16 , wherein the tuning parameters are functions of geographic coordinates.