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Abstract The probability of the concordance of a geological section with reality has been defined as the reverse of the number of all possible geological sections that can be created on the basis of all the geological data collected. The five kinds of geological sections ave distinguished: fully hypothetical, partly hypothetical, probable, generally credible and fully credible. The interdependence between the geological probability of sections and the number of fully worthwhile geological data is pointed out. This geological probability of the sections, as well as the model of the geological structure, increase at every stage of the engineering-geological studies and in the end it ought to be 1 in the engineering-geological elaboration for the technical project.
Abstract The probability of the concordance of a geological section with reality has been defined as the reverse of the number of all possible geological sections that can be created on the basis of all the geological data collected. The five kinds of geological sections ave distinguished: fully hypothetical, partly hypothetical, probable, generally credible and fully credible. The interdependence between the geological probability of sections and the number of fully worthwhile geological data is pointed out. This geological probability of the sections, as well as the model of the geological structure, increase at every stage of the engineering-geological studies and in the end it ought to be 1 in the engineering-geological elaboration for the technical project.
Geological section probability
Kowalski, W. C. (author)
1983
Article (Journal)
English
Boulder , Geological Data , Clay , Engineer Geology , Gravel
Geological section probability
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