Evidence item
The peer-reviewed study identifies at least three alteration episodes in the Margin unit. DIRECT_TEXT
Source: Lake- and groundwater-associated alteration of the olivine-rich Margin unit in Jezero crater, Mars · locator {} · excerpt hash sha256:f7de17cd36bea632363b0654f81266fdcdbe1c55112b7b0057f3ff181f5b2e6c
Exact excerpt
Following emplacement, the Margin unit experienced at least three episodes of alteration: 1) neutral-to-alkaline, CO2-rich meteoric fluids formed carbonate-rich fracture fill that later eroded into ridges; 2) lower-pH solutions remobilized carbonate, driving secondary porosity generation and silica precipitation from cooler and/or silica-saturated fluids; and 3) late-stage hydrothermal fluids flowed through younger fractures, precipitating Ca-sulfate-rich and fluorite-bearing mineral veins.
Linked claims
| Claim | Direction | Relevance | Steps | Counted |
|---|---|---|---|---|
| 0aee692c | SUPPORT | DIRECT | 0 | yes |
Audits
None.