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...
שמור ב:
| Principais autores: | , , , , |
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| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Wiley
2025-12-01
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| סדרה: | Geochemistry, Geophysics, Geosystems |
| נושאים: | |
| גישה מקוונת: | https://doi.org/10.1029/2025GC012638 |
| תגים: |
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