Diagenetic, Nonevaporative Origin for Calcium Sulfate Salts at Gale Crater
Abstract Sulfate salts are deposited most commonly as evaporites on Earth; however, this is not their only origin. Pyrite oxidation during subsurface weathering is another common process on Earth that also produces a suite of sulfate salts—including the acidic phases jarosite and alunite—in sediment...
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| Principais autores: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Wiley
2025-12-01
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| Series: | Geochemistry, Geophysics, Geosystems |
| Assuntos: | |
| Acceso en liña: | https://doi.org/10.1029/2025GC012638 |
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