Titlebook: Geostatistics for the Next Century; An International For Roussos Dimitrakopoulos Book 1994 Springer Science+Business Media Dordrecht 1994 e

太空

伦理学

Facilities

Reply to “Comment on Estimating or Choosing a Geostatistical Model” by M.S. Handcock from one perspective appears to be knowledge from another”. Uncertainty quantification is usually achieved through the use of a probabilistic model. Too often, the geologist is not asked the right questions by the geostatistician. For instance, if the problem is probabilistic heterogeneity modellin

Prologue

VEIL

Modeling Uncertainty: Some Conceptual Thoughtsr decisions about the randomization of either the unknown itself and/or its estimate and, as such, cannot claim to any objectivity. A safeguard for building such models is to charge them maximally with data deemed relevant to the “unknown” at hand..Another look at Bayes’ relation shows that its prac

escalate

The Role of Massive Grade Data Bases in Geostatistical Applications in South African Gold Minescs is covered briefly. The continuation of this role throughout and particularly during the last decade is dealt with in more detail. It is shown how this has led to the development of new distribution models and also to studies of the regional variations in the parameters of the distributions and s

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Multiple Indicator Kriging of Precious Metals at Silbak Premier Mine, British Columbiaith emphasis on post1980 data; limited use of blastnole assays from open pit operations during 1990-91 was essential to our structural analysis. Within a mineralized zone the downhole grade distribution is highly erratic in that single high assays can be contiguous with low grade assays. Thus, a hig

browbeat

BRIDE

Joint Temporal-Spatial Modeling of Concentrations of Hazardous Pollutants in Urban Airnts in urban air. The objective of this analysis is to determine how reliably concentrations measured at one or more times and locations can be used to estimate concentrations at other times and locations. The approach used is that of classical three-dimensional ordinary kriging with a joint tempora

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