INTENSE PYRITE FORMATION UNDER LOW-SULFATE CONDITIONS IN THE ACHTERWASSER LAGOON, SW BALTIC SEA
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Neumann T. | |
dc.contributor.author | Rausch N. | |
dc.contributor.author | Berner Z. | |
dc.contributor.author | Leipe T. | |
dc.contributor.author | Dellwig O. | |
dc.contributor.author | Böttcher M.E. | |
dc.date.accessioned | 2023-11-26T02:22:44Z | |
dc.date.available | 2023-11-26T02:22:44Z | |
dc.date.issued | 2005 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14610766 | |
dc.identifier.citation | Geochimica et Cosmochimica Acta, 2005, 69, 14, 3619-3630 | |
dc.identifier.issn | 0016-7037 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/42022 | |
dc.description.abstract | In comparison to similar low-sulfate coastal environments with anoxic-sulfidic sediments, the Achterwasser lagoon, which is part of the Oder estuary in the SW Baltic Sea, reveals unexpectedly high pyrite concentrations of up to 7.5 wt%. Pyrite occurs mainly as framboidal grains variable in size with diameters between 1 and 20 μm. Pyritization is not uniform down to the investigated sediment depth of 50 cm. The consumption of reactive-Fe is most efficient in the upper 20 cm of the sediment column, leading to degrees of pyritization (DOP) as high as 80 to 95%. | |
dc.title | INTENSE PYRITE FORMATION UNDER LOW-SULFATE CONDITIONS IN THE ACHTERWASSER LAGOON, SW BALTIC SEA | |
dc.type | Статья | |
dc.identifier.doi | 10.1016/j.gca.2005.02.034 |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru