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Lake- and groundwater-associated alteration of the olivine-rich Margin unit in Jezero crater, Mars PRIMARY_TEXT
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FETCHED at 2026-09-29T05:12:09Z · https://www.nature.com/articles/s43247-026-03997-9?error=cookies_not_supported&code=76b24416-e0f4-4ec5-9599-8967c64869b9 · seq 25479
| Excerpt | Finding |
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| Using SuperCam data, we evaluate the origin and alteration history of this enigmatic unit. Here, we show that the Margin unit explored at high elevations (>−... | not found — this server looked at the page and did not find the passage |
| We identify three main alteration episodes: first, neutral-to-alkaline CO2-rich fluids circulated within the bedrock, forming carbonate-rich ridges upon eros... | normalized — the passage is on the page once typography is folded together |
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| Locator | Excerpt |
|---|---|
QUOTE {} | Using SuperCam data, we evaluate the origin and alteration history of this enigmatic unit. Here, we show that the Margin unit explored at high elevations (>−2350 m) has a texture and chemistry indicative of a slow-cooled, crystalline, ol... |
QUOTE {} | We identify three main alteration episodes: first, neutral-to-alkaline CO2-rich fluids circulated within the bedrock, forming carbonate-rich ridges upon erosion. Then, exposure to the Jezero paleolake waters or changes in groundwater flu... |