Titlebook: Geostatistics Rio 2000; Proceedings of the G M. Armstrong,C. Bettini,A. Remacre Conference proceedings 2002 Springer Science+Business Media

注意

Geostatistical Evaluation of the Mineral Resources of the Cajati Mine, State of S?o Paulo, Brazilied separately. The statistical analysis also showed that the correlation between the two variables was very low so they were studied separately. Then the variograms were computed and modelled. Ordinary kriging was used to estimate the grades of both variables in mining blocks of 25 m X 25 m X 10 m

大洪水

Variographic Trends of Gold in the Alluvial Sediments Associated with the Quartz Lodes of the Princeariogram resulted in an acceptable model with a sample range of 7 m. The directional variographic analysis showed the presence of a well-defined structure and a systematic variation in the assay values. Continuity and spatial correlation between the sample gold assays can be detected in the variogra

jarring

Defense

British Petroleum Deepwater Horizon,sited in a low accommodation context are different from those deposited in a high one. These curves can also show up possible errors in the correlation or in the determination of the reference level..Horizontal proportion curves represent the lateral evolution of the amount of lithofacies. They are

Lipoma

彎彎曲曲

Tankiso Moloi,Tshilidzi Marwalancorporated into a gaussian stochastic model in order to characterise the reservoir and then the fluid flow is simulated..The sand percentage estimated from the seismic attributes can be introduced into the stochastic model. The models with and without seismic constraints are compared first from a g

側(cè)面左右

Auf dem Weg zur vernetzten Organisationplurigaussian simulation method. When applying this methodology, the key steps are:.We describe how these steps were applied to the Rossing data, emphasising the geologist’s input into the decision-making process. Several simulations were generated.

Blatant

開(kāi)玩笑

Evolution of Enterprise Systemstatistical evaluation. Two distinct geological domains were defined, resulting in two sub-datasets. Samples available from auger holes were logged and analysed at different lengths (support), requiring the use of accumulations to overcome the problem caused by multiple sample supports..Ordinary krig

OATH

Ein Meeting zur Wiki-Philosophieon techniques to evaluate the uncertainty involved in each of these phases. The role of each component of spatial uncertainty given by the simulation models (the lack of knowledge about the physical phenomenon and intrinsic variability of the orebody variables) in those decisions, is evaluated by co