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Mineralogy of a Mudstone at Yellowknife Bay, Gale Crater, Mars

2013· article· en· 667 citations· W2011543988 on OpenAlex· 10.1126/science.1243480

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Opus teacher head0.009
GPT teacher head0.215
Teacher spread
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Validation status
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Abstract

Sedimentary rocks at Yellowknife Bay (Gale crater) on Mars include mudstone sampled by the Curiosity rover. The samples, John Klein and Cumberland, contain detrital basaltic minerals, calcium sulfates, iron oxide or hydroxides, iron sulfides, amorphous material, and trioctahedral smectites. The John Klein smectite has basal spacing of ~10 angstroms, indicating little interlayer hydration. The Cumberland smectite has basal spacing at both ~13.2 and ~10 angstroms. The larger spacing suggests a partially chloritized interlayer or interlayer magnesium or calcium facilitating H2O retention. Basaltic minerals in the mudstone are similar to those in nearby eolian deposits. However, the mudstone has far less Fe-forsterite, possibly lost with formation of smectite plus magnetite. Late Noachian/Early Hesperian or younger age indicates that clay mineral formation on Mars extended beyond Noachian time.

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The record

Venue
Science
Topic
Planetary Science and Exploration
Field
Physics and Astronomy
Canadian institutions
Funders
Keywords
GeologyNoachianGeochemistryClay mineralsHesperianBasaltSedimentary rockMars Exploration ProgramMineralForsteriteImpact craterMineralogyMartianAstrobiologyChemistry
Has abstract in OpenAlex
yes