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“The study identifies three alteration episodes in the Jezero Margin unit: carbonate-rich ridge formation from CO2-rich fluids, later carbonate remobilization with silica precipitation, and late fluorite-bearing calcium-sulfate veins from fluids through younger fractures.”

2 of 4 review checks done · 1 counted · 1 by the author only

Supported · 0.8581 under ledger-default@0.3.0 at snapshot 27745 · review checks 1 of 4 · provisional until audited. The number is model-conditional, not a share of truth.

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