Author(s): Giorgi Mindiashvili* and Davit Bluashvili
Discontinuities, distribution scales and formation conditions of Adjara-Trialeti Gujareti-Tskarostavi ore field are reviewed in the work. As known, studying ore field structures has got big significance for increasing efficiency of investigation works. Gujareti-Tskarostavi ore field is highly complicated by tectonic viewpoint. Various type dysunctives and fractures are observed. Part of fold structures, Arjevani-Bakuriani fault and other geological elements in distribution of ore field is represented in the article. Characterization of ore column structures has got big part, which is connected to magmatic creatures, fold forms and discontinuities. Basic and specialized methods of studying structures are used in the work.
Besides, Gujareti-Tskarostavi ore field was studied by us with distant probing method, resulted of which basic fault and stress structures were revealed, where the best conditions are made for establishment of ore field. In particular, adjacent territory of Arjevani-Bakuriani fault represents convenient conditions for oreing-down.
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