A set of straight lines defined by their end points define the pillars of the corner-point grid. The pillars have a lexiographical ordering that determines neighbouring pillars. On each pillar, a constant number of nodes (corner-points) is defined. A corner-point cell is now the volume between 4 neighbouring pillars and two neighbouring points on each pillar.
Each cell can be identified by integer coordinates \((i,j,k)\), where the \(k\) coordinate runs along the pillars, and \(i\) and \(j\) span each layer. The cells are ordered naturally, where the index \(i\) runs the fastest and \(k\) the slowest.
Corner-point grids are supported by most reservoir simulation software, and has become an industry standard.
A main feature of the format is the ability to define erosion surfaces in geological modelling, effectively done by collapsing nodes along each pillar. This means that the corner-point cells degenerate and may have less than 6 faces.
For the corner-point grids non-neighboring connections are supported, meaning that grid cells that are not neighboring in ijk-space can be defined as neighboring. This feature allows for representation of faults with significant throw/displacement. Moreover, the neighboring grid cells do not need to have matching cell faces (just overlap).
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