Rare earth elements and yttrium in calcite and pyrite of the Orlovka gold deposit (the Southern Urals)
REE and Y patterns for calcite and pyrite of the Orlovka gold deposit were considered. Two environments, in which evolved ore-forming fluid, are determined: early high-temperature (>200-250ºC) and later low-temperature (
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| Format: | Article |
| Language: | English |
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A.N. Zavaritsky Institute of Geology and Geochemistry
2017-02-01
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| Series: | Литосфера |
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| Online Access: | https://www.lithosphere.ru/jour/article/view/77 |