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During the last period is modern geology oriented toward intensive utilisation of mathematical methods. Utilisation of these methods was conditioned by complicated structure of geological bodies, which resulted from interaction of a couple of factors. In the period of projection, realisation and evaluation of geological works one meet many problems of description of a character of geological data. These problems very often trivial arise from the poor knowledge of the principles of statistical methods. Transformation of real geological object into the form of abstract mathematical model is the basic and usually also the most complicated step of mathematical solution. There is also to be mentioned that there is no unitary approach to the modelling or uniform direction for a method of data processing selection. Complicacy of geological objects needs rational simplification of the model, otherwise the solution would be too complicated or even impossible.
During the last period is modern geology oriented toward intensive utilisation of mathematical methods. Utilisation of these methods was conditioned by complicated structure of geological bodies, which resulted from interaction of a couple of factors. In the period of projection, realisation and evaluation of geological works one meet many problems of description of a character of geological data. These problems very often trivial arise from the poor knowledge of the principles of statistical methods. Transformation of real geological object into the form of abstract mathematical model is the basic and usually also the most complicated step of mathematical solution. There is also to be mentioned that there is no unitary approach to the modelling or uniform direction for a method of data processing selection. Complicacy of geological objects needs rational simplification of the model, otherwise the solution would be too complicated or even impossible.
Mathematical Statistics in the Geology
Blišťan Peter (author)
1999
Article (Journal)
Electronic Resource
Unknown
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