| Reference Type | Journal (article/letter/editorial) |
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| Title | Fossilized Bacteria in Fe-Mn-Mineralization: Evidence from the Legrena Valley, W. Lavrion Mine (Greece) |
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| Journal | Minerals |
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| Authors | Vasilatos, Charalampos | Author |
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| Economou-Eliopoulos, Maria | Author |
| Year | 2018 (March 8) | Volume | < 8 |
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| Page(s) | 107 | Issue | < 3 > |
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| Publisher | MDPI AG |
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| URL | |
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| DOI | doi:10.3390/min8030107Search in ResearchGate |
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| Original Entry | Vasilatos, Charalampos, and Maria Economou-Eliopoulos (2018) Fossilized Bacteria in Fe-Mn-Mineralization: Evidence from the Legrena Valley, W. Lavrion Mine (Greece). Minerals 8, no. 3: 107. https://doi.org/10.3390/min8030107 |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 16375109 | Long-form Identifier | mindat:1:5:16375109:6 |
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| GUID | d7c69ea1-e4fb-450d-976c-ce519afdbc5e |
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| Full Reference | Vasilatos, Charalampos, Economou-Eliopoulos, Maria (2018) Fossilized Bacteria in Fe-Mn-Mineralization: Evidence from the Legrena Valley, W. Lavrion Mine (Greece) Minerals, 8 (3) 107 doi:10.3390/min8030107 |
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| Plain Text | Vasilatos, Charalampos, Economou-Eliopoulos, Maria (2018) Fossilized Bacteria in Fe-Mn-Mineralization: Evidence from the Legrena Valley, W. Lavrion Mine (Greece) Minerals, 8 (3) 107 doi:10.3390/min8030107 |
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| In | Link this record to the correct parent record (if possible) |
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| Abstract/Notes | The primary mineralization in the famous Lavrion mine in the Lavreotiki area, Attica (Greece), associated with a granodiorite intrusion of Upper Miocene age and composed of massive sulphide Pb-Zn-Ag ores [sphalerite, pyrite and galena (B.P.G)], has been extensively studied. The present study is focused on thin, hard, dark brown to black Fe-Mn crusts (a few mm to cm in thickness) in the Legrena valley, SW Lavreotiki, aiming to provide new insights on that type of Fe-Mn-mineralization. The scanning electron microscope (SEM)/energy dispersive spectroscopy (EDS) data presented revealed the presence of fine rounded fragments, resembling nodules (up to 200 μm) and fossilized bacteriomorphic Fe-Mn-oxides/hydroxides, within brecciated and foliated zones of carbonate rocks. They exhibit unusual features when compared to the common massive Fe-Mn mineralization with regards the following: (a) the extensive occurrence of bacteriomorphic Fe-oxides/hydroxides and their micro-textures; and (b) the minor elements (K, Na, P, S, Ca, As and Cl). The occurrence of abundant bacteriomophic Fe-Mn-oxides/hydroxides in the samples from the Legrena valley may reflect their catalytic role in the redox reactions during ore-forming processes. The characteristic features of that type of Fe-Mn mineralization seems to be the result of multistage supergene processes superimposed over initial hydrothermal stages. Such a multistage remobilization and precipitation of metals along open space surfaces on karstified carbonates during a subsequent stage of their initial precipitation may be widespread in the Attica region, Greece. |
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