Classically, the non stationary lithofacies distribution inside reservoirs is described by the 3D distribution of their proportions. This approach is very attractive because proportions have a physical meaning. Moreover their 3D distribution reflects the qualitative...
CITATION STYLE
Beucher, H., García-Morales, M., & Geffroy, F. (2005). Fitting the Boolean Parameters in a Non-stationary Case (pp. 569–578). https://doi.org/10.1007/978-1-4020-3610-1_58
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