Evaluation of geoinformation has been discussed in order to optimize a geoscience survey. The discussion suggests that 1) geoinformation can be evaluated by either of variance or entropy, and 2) entropy is more advantageous, because, if a target area consists of many geologic units, entropy diverges with increasing number of geologic units, but variance converges. A simple model suggests a probability that surveying a narrow area with a high resolution technique is rarely more advantageous than surveying a wide area with a low resolution technique. The model suggests that low resolution techniques are applied at early stages of a survey, and that higher resolution techniques should alternate them with progressing survey.
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