Three dimensional geological model construction
A method for modeling geological structures includes identifying fault planes in a geologic structure, and creating a set of substantially vertically oriented pillars along the fault plane. The pillar grids are then combined into a common three-dimensional grid pillar network, and a two-dimensional plane is defined that intersects the middle node of the pillars. Planes are identified that are oriented in the substantially horizontal direction and horizontal node points are created, and such a process is repeated for other node levels. A skeleton grid is then created by drawing a substantially vertically oriented pillar through each corresponding grid intersection, and then primary horizons as defined by interpretation of seismic data are inserted into the skeleton grid. And, a final scale resolution is created by dividing the spaces bounded between actual horizons and fault planes, and eventual actual part of the outer boundary into one or more horizontally oriented fine layers.
1. A method for modeling geological structures, where faults, horizons and zones within the geologic structure are modeled by a common framework using a three-dimensional grid of pillars, characterized in that the method comprises the steps of:
A) identifying all fault planes in the geologic structure by interpreting information pertaining to the geologic structure, wherein the identified fault planes each have a base level, middle level and top level;
B) creating a set of substantially vertically oriented (z-direction) pillars along each identified fault plane, where each pillar is defined by at least three node points that intersect the fault plane at the base level, middle level and top level of fault plane, such that a series of pillars that corresponds to the geometry of the fault plane are created for each fault plane in the geologic structure that is to be modeled, and so that the combination of the pillars with each of the fault planes becomes a pillar grid;
C) combining the pillar grids of each fault plane into a common three-dimensional grid pillar network that provides a realistic representation of the geometry of the fault planes in the geologic structure that is to be modeled,
D) defining a two-dimensional plane that intersects the node at the middle level of each pillar in the three-dimensional grid pillar network representing the fault planes, and where the outer boundary of the two-dimensional plane are given by an arbitrarily drawn closed curve that defines an area that at least covers the area of the three-dimensional grid pillar network representing the fault planes when projected onto a horizontal plane, such that the two-dimensional plane is divided into a set of horizontally oriented sub-zones bounded by the corresponding fault planes and part of the outer boundary,
E) identifying the fault planes that are oriented in the substantially horizontally i- and j-direction respectively, and creating a two-dimensional network of grip lines in i- and j-direction in each sub-zone bounded by the corresponding fault planes and outer boundary,
F) creating horizontal node points, at intersections between i- and j-lines, such that i- and j-lines are made as perpendicular to each other as possible and such that the area of each cell defined by the two-dimensional network are made as equal as possible,
G) repeating steps D) and F) for the base level and top level of node points of the three-dimensional grid pillar network representing the fault planes, such that corresponding substantially horizontally oriented two-dimensional sub-zones are created for at least the base-, middle- and top-level of the three-dimensional grid pillar network representing the fault planes,
H) creating a skeleton grid by drawing a substantially vertically oriented pillar through each corresponding grid intersections in the at least base-, middle-, and top two-dimensional grid representing the horizontally oriented two-dimensional sub-zones, thus creating a vertically oriented pillar network that represents the space between the corresponding bounding fault planes and part of the outer boundary as defined by the arbitrarily drawn closed curve for each sub-zone,
I) inserting all primary horizons as defined by interpretation of information pertaining to the primary horizons into the skeleton grid such that the horizons are placed correctly in relation the fault planes, and define the vertical coordinate of each primary horizon node as the intersection between the actual horizon plane and skeleton pillar,
J) repeating step I) for all geological zones as determined by the interpretation of information pertaining to the geological zones such that a complete geological description of the geologic structure that is to be modeled is formed, and
K) creating final scale resolution by dividing all spaces bounded between actual horizons and fault planes, and eventual actual part of outer boundary into one or more horizontally oriented fine layers.
2. Method according to claim 1 , characterized in that the thicknesses of the geological zones are given as isochors, surfaces representing the vertical thickness in each zone.
3. Method according to claim 1 , characterized in that the thicknesses of the geological zones are given as isopachs, surfaces representing the stratigraphic thickness of each zone.
4. Method according to claim 1 , characterized in that the thicknesses of the geological zones are given as constant values, as an absolute number or percentage of the total thickness of the actual zone.
5. Method according to any one of claims 1 to 4 , characterized in that the fine layering is performed by adding layers from base to top of each geological zone by using constant thickness and truncating at the top layer.
6. Method according to any one of claims 1 to 4 , characterized in that the fine layering is performed by adding layers by proportional thickness using a specified number of fine layers in each geological zone.
7. Method according to any one of claims 1 to 4 , characterized in that the fine layering is performed by adding layers from base to top of the geological zone using a dipping surface.