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...
Gorde:
| Egile Nagusiak: | , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Wiley
2025-12-01
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| Saila: | Geochemistry, Geophysics, Geosystems |
| Gaiak: | |
| Sarrera elektronikoa: | https://doi.org/10.1029/2025GC012638 |
| Etiketak: |
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