Process for three-dimensional mathematical modeling of underground geologic volumes

Claim 2

A process for modeling a geologic volume bounded by critical surfaces, the volume having a given geologic stratigraphic pattern, other than a volume having depositional layers parallel to mean sea level, the process comprising the steps of: a. constructing a separate grid for each critical surface bounding said volume; and b. constructing layers of cells within said volume according to said pattern.

Claim 3

A process for modeling a stratigraphic geologic subvolume including an inclined initiating surface, a limiting surface and layers of sediments spanning an interval of geologic time occupying the space between said surfaces, which comprises: dividing said space into a plurality of laterally disposed, laterally aligned and vertically spaced grids of elemental cells, each cell having a reference point at each of its corners, the reference points in each said grid positioned to be along a grid layer of sediments of the same geologic time and to be equally spaced horizontally from each laterally adjacent reference point in said grid; vertically spacing said grids such that each said reference point in a vertical column of reference points is equidistant from each next adjacent reference point in said column; assigning representative x, y, z coordinates to each said reference point such that each elemental cell in said space may be identified by the sets of said coordinates at its respective corners; and reproducibly recording said sets of coordinates in digital form.

Claim 4

A process for modeling a stratigraphic geologic subvolume including an inclined initiating surface, a limiting surface and layers of sediments spanning an interval of geologic time occupying the space between said surfaces, which comprises: dividing said space into a plurality of laterally disposed, laterally aligned and vertically spaced grids of elemental cells, each cell having a reference point at each of its corners, the reference points in each said grid positioned to be along a grid layer of sediments of the same geologic time and to be equally spaced horizontally from each laterally adjacent reference point in said grid; vertically spacing said grids such that each said reference point in a vertical column of reference points is equidistant from each next adjacent reference point in said column; assigning representative x, y, z coordinates to each said reference point such that each elemental cell in said space may be identified by the sets of said coordinates at its respective corners; and reproducibly recording said sets of coordinates in digital form.

Claim 5

The method of claim 2 in which a characteristic of a given said elemental cell is stored in digital form in association with a set of said coordinates for said given cell.

Claim 6

The method of claim 3 further comprising the step of reproducing said characteristic and visually displaying said reproduced characteristic.

Claim 7

The method of claim 2 in which said subvolume is an onlap sequence, or an offlap sequence, or a truncation sequence, and all of said reference points in any given laterally disposed layer are equidistant from their vertically corresponding reference points in vertically adjacent said grids.

Claim 8

A process for modeling a geologic subvolume including an inclined originating surface, a limiting surface, and layers of sediments spanning an interval of geologic time occupying the space between said surfaces, which comprises: (1) dividing said space into a plurality of cells by (a) constructing a grid for said originating surface; (b) constructing layers of laterally disposed cells from said grid, the cells in successive said layers aligned in vertical columns; (2) assigning a set of coordinates to each said cell, whereby each said cell may be identified by its respective coordinates; (3) reproducibly and systematically recording said sets of coordinates; and (4) reproducibly recording a characteristic of a given cell in association with the coordinates of said given cell.

Claim 9

A process for modeling a geologic subvolume including an inclined originating surface, a limiting surface, and layers of sediments spanning an interval of geologic time occupying the space between said surfaces, which comprises: (1) dividing said space into a plurality of cells by (a) constructing a grid for said originating surface; (b) constructing layers of laterally disposed cells from said grid, the cells in successive said layers aligned in vertical columns; (2) assigning a set of coordinates to each said cell, whereby each said cell may be identified by its respective coordinates; (3) reproducibly and systematically recording said sets of coordinates; and (4) reproducibly recording a characteristic of a given cell in association with the coordinates of said given cell.

Claim 10

The method of claim 6 in which said characteristic is vertical distance from a datum level.

Claim 11

The method of claim 7 in which said vertical distance is recorded for each said set of reference coordinates, and which includes the steps of reproducing in visual map form all of said points whose sets of coordinates lie at a selected vertical distance from said datum level.

Claim 12

The method of claim 6 which includes reproducing in visual section form all of said points whose sets of coordinates lie in a common vertical plane passed through said space.

Claim 13

A process for modeling a bounded geologic volume, other than a volume having depositional layers parallel to mean sea level, having a given geologic stratigraphic pattern and a given initiating critical surface, comprising the steps of: (a) constructing a separate grid for each critical surface bounding said volume; and (b) constructing layers of cells between said grids and substantially parallel to said given initiating critical surface.

Claim 14

A process for modeling a bounded geologic volume, other than a volume having depositional layers parallel to mean sea level, having a given geologic stratigraphic pattern and a given initiating critical surface, comprising the steps of: (a) constructing a separate grid for each critical surface bounding said volume; and (b) constructing layers of cells between said grids and substantially parallel to said given initiating critical surface.

Claim 15

The process of claim 10 in which said given initiating critical surface is a naive surface.

Claim 22

The method of claim 14, including the step of systematically and retrievably storing the cell coordinates.

Claim 23

The method of claim 15, including the step of retrievably storing an observation obtained at a given position within the geologic volume according to the cell coordinates of the cell corresponding to the given position within the geologic volume.