File:Volkanojenik Masif Sülfit Maden Yatağı Profil Kesiti.png
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Türkçe: Bu, tipik bir volkanojenik masif sülfit (VMS) cevher yatağının bir kesitidir. Bir ekzalit veya tüfit, hidrotermal sıvıların etkisiyle deniz suyundan biriken tortudan oluşur. Paleo-deniz tabanındaki ekzalit, genellikle, keşif için yararlı olan kaynak menfezine doğru doğrultu boyunca takip edilebilir. Altta yatan daha eski volkanik kayaçlar, doğrudan mineralizasyon kaynağı değildir. cpy=kalkopirit py=pirit po=pirotit sp=sfalerit gn=galen ba=barit. Daha fazla bilgi için bkz. Hannington, M.D. (2014). "Volkanojenik masif sülfür yatakları". Jeokimya Üzerine İnceleme (İkinci Baskı) 13: 463-488. DOI: https://doi.org/10.1016/B978-0-08-095975-7.01120-7. |
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| Source | https://en.wikipedia.org/wiki/Volcanogenic_massive_sulfide_ore_deposit |
| Author | RockingGeo |
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| current | 08:37, 7 April 2023 | | 1,489 × 1,369 (257 KB) | Ozgurydk (talk | contribs) | Uploaded a work by RockingGeo from https://en.wikipedia.org/wiki/Volcanogenic_massive_sulfide_ore_deposit with UploadWizard |
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