Abstract:
Lithofacies maps display spatial changes in the lithological composition of rocks
and the direction of their replacement characteristics for
a certain geological time depending on the physical and geographical
conditions of their sedimentation. Lithofacies maps are constructed
based on the analysis of complexes of genetically related deposits with
characteristic material features of lithofacies. The initial data can be
either only points on a plane — well coordinates where certain lithofacies occur
— or additionally a map of sediment accumulation rates.
It is assumed that identical facies should have similar sedimentation
rates. The task of constructing a lithofacies map is to determine the
boundaries of facies distribution areas. The paper proposes to reduce
the map construction problem to the graph coloring problem, which in
turn is solved using integer linear programming methods. This approach
allows us to automatically construct realistic maps – that is, maps that
satisfy expert constraints and rules.