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Publikováno v:
Chemical Geology. 468:42-48
The iron sulfide mineral greigite, Fe 3 S 4 , has previously been identified in the surface layers of the intertidal zone of a partially remediated acid sulfate soil wetland, representing an end-member in an iron sulfide mineralization pathway distin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e22d8fe3634713ee143e46dc5166107
https://doi.org/10.1016/j.chemgeo.2017.08.007
https://doi.org/10.1016/j.chemgeo.2017.08.007
