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It is shown that in model-based geostatistics, not all parameters in the Matérn class can be estimated consistently if data are observed in an increasing density in a xed domain, regardless of the estimation methods used. Nevertheless, one quantity can be estimated consistently by the maximum likelihoodmethod, and this quantity is more important to spatial interpolation. The results are established by using the proper-ties of equivalence and orthogonality of probability measures. Some suf cient conditions are provided for both Gaussian and non-Gaussian equivalent measures, and necessary conditions are provided for Gaussian equivalent measures. Two simulation studies are presented that show that the xed-domain asymptotic properties can explain some nite-sample behavior of both interpolation and estimation when the sample size is moderately large.
Hao Zhang (Mon,) studied this question.
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