Minerals, native metals, and intermetallides in bottom sediments of the Markov Deep, Mid-Atlantic Ridge
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| Auteurs principaux: | , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2006
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| _version_ | 1867168561575755776 |
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| author | Bortnikov, Nikolay S Mochalov, A G Cherkashov, Georgy A |
| author_facet | Bortnikov, Nikolay S Mochalov, A G Cherkashov, Georgy A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Bottom sediments of the Markov Deep contain rather large (>0.1 mm) grains of native minerals and intermetallides of noble and nonferrous metals that can be concentrated in placers. Intermetallides of Pt and Fe are likely to be derivates of the gold-hematite-barite assemblage that forms at late (low-depth) stages of hydrothermal massive sulfide formation. Mineral association of native forms of lead, tin, and copper with Zn-bearing copper may be related to hydrothermal transformation of ultrabasic and basic rocks accompanied by massive sulfide copper mineralization. The association of these minerals of native elements in bottom sediments can also serve as a prospecting guide for sulfide mineralization both at the Sierra Leone site, in particular, and on the seafloor, in general. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_788240 |
| institution | PANGAEA |
| language | en |
| publishDate | 2006 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Minerals, native metals, and intermetallides in bottom sediments of the Markov Deep, Mid-Atlantic Ridge Bortnikov, Nikolay S Mochalov, A G Cherkashov, Georgy A Archive of Ocean Data; ARCOD Bottom sediments of the Markov Deep contain rather large (>0.1 mm) grains of native minerals and intermetallides of noble and nonferrous metals that can be concentrated in placers. Intermetallides of Pt and Fe are likely to be derivates of the gold-hematite-barite assemblage that forms at late (low-depth) stages of hydrothermal massive sulfide formation. Mineral association of native forms of lead, tin, and copper with Zn-bearing copper may be related to hydrothermal transformation of ultrabasic and basic rocks accompanied by massive sulfide copper mineralization. The association of these minerals of native elements in bottom sediments can also serve as a prospecting guide for sulfide mineralization both at the Sierra Leone site, in particular, and on the seafloor, in general. |
| title | Minerals, native metals, and intermetallides in bottom sediments of the Markov Deep, Mid-Atlantic Ridge |
| topic | Archive of Ocean Data; ARCOD |
| url | https://doi.org/10.1594/PANGAEA.788240 |