Source
Lake- and groundwater-associated alteration of the olivine-rich Margin unit in Jezero crater, Mars PRIMARY_TEXT retrieval pending
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QUOTE {} | The Margin unit explored at high elevations (>−2350 m) has a texture and chemistry indicative of a slow-cooled, crystalline, olivine-rich rock without significant water exposure. In contrast, exposures situated below the hypothesized Jez... |