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dc.contributor.author Rickard D.
dc.contributor.author Iii G.W.L.
dc.date.accessioned 2025-04-19T06:19:25Z
dc.date.available 2025-04-19T06:19:25Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=14668956
dc.identifier.citation Reviews in Mineralogy and Geochemistry, 2006, 61, 61. С. 4, 421-504
dc.identifier.issn 1529-6466
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48941
dc.description.abstract The metal chemistry of anoxic systems is dominated by reactions with reduced sulfur species. These reduced sulfur systems presently characterize the Earth’s subsurface and are occasionally important in marine and freshwater systems. In the first half of Earth history, of course, the surface environments were also anoxic and the reduced sulfur chemistry played an even more widespread role in the geochemistry of base metals.
dc.title METAL SULFIDE COMPLEXES AND CLUSTERS
dc.type Статья
dc.identifier.doi 10.2138/rmg.2006.61.8


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