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...
Sábháilte in:
| Príomhchruthaitheoirí: | , , , , |
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| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe / Cruthaithe: |
Wiley
2025-12-01
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| Sraith: | Geochemistry, Geophysics, Geosystems |
| Ábhair: | |
| Rochtain ar líne: | https://doi.org/10.1029/2025GC012638 |
| Clibeanna: |
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
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