| Define faults and breaklines when gridding your data. The
data on one side of the fault will not be directly used to calculate grid node
values on the other side of the fault. When the gridding algorithm sees a
breakline, any data points that lie directly on the breakline take precedence
over an interpolated value. Use breaklines to define streamlines, ridges, and
other breaks in slopes. Unlike faults, breaklines are not barriers to
information flow and the gridding algorithm can cross the breakline to use a
point on the other side. The gridding methods that support faults are: Inverse
Distance to a Power, Minimum Curvature, Nearest Neighbor, and Data Metrics.
Breaklines are supported by: Inverse Distance to a Power, Kriging, Minimum
Curvature, Nearest Neighbor, Radial Basis Function, Moving Average, Data
Metrics, and Local Polynomial gridding methods.
A contour map that features
a fault is displayed here. Faults and breaklines are specified when gridding
your data
|
|
|