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Towards the question of the movement of hydrothermal solutions: The case of the Schlema-Alberoda vein deposit |
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| Authors: | G B Naumov B P Vlasov O F Mironova |
| Institution: | 1. Vernadsky State Geological Museum, Russian Academy of Sciences, Mokhovaya ul., 11, korp. 11, Moscow, 125009, Russia 2. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, Staromonetnyi per. 35, Moscow, 119017, Russia 3. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, pr. Kosygina 19, Moscow, 119991, Russia |
| Abstract: | The paths of the movements of hydrothermal solutions are considered in the case of one of the world’s largest uranium vein deposits, the Schlema-Alberoda, which was mined by the Soviet-German corporation Wismut JSC in the second half of the 20th century. Detailed geological exploration to a depth of 2 km was accompanied by specialized research, the results of which have remained practically unpublished due to confidentiality. The data obtained show that the region adjoining the largest fault was draining rather than ore-conducting. This circumstance specifies and supplements the current concept concerning the movement of hydrothermal fluids. |
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