Determination of the degree of similarity of geologic structures
Abstract
Assessment of the degree of similarity or difference of geological structures has always been of interest to researchers, as it has practical implications: questions of the genesis of structures and predictions of the distribution of mineral deposits are largely solved taking into account possible analogies. The complexity of this assessment is compounded by the fact that natural objects, unlike the products of human technological activity, are in their individual features necessarily unique. Even in the simplest cases, one can reasonably expect some difference between nearby structures having the same origin. A significant difficulty is the selection of those indicators (attributes) by which the degree of closeness of the compared geological structures is assessed. Heightened interest in certain aspects (genesis, ore content, metamorphism, etc.) may manifest itself in the fact that some features will subjectively receive greater importance than others, while some will be entirely omitted from the analysis.
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